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PopupWebFrameBehaviour_F21DB74A_F403_49EB_41DF_D184CF0088AF.url = //www.youtube.com/embed/s_dm6K7sPuA?rel=0&autoplay=1 VideoUrl_07681EF3_06F8_B474_419D_46BF5AE5B065.url = //www.youtube.com/embed/sfp5KXNkqp0?rel=0&autoplay=1 VideoUrl_07681EF3_06F8_B474_418D_FC8C01C7FF47.url = //www.youtube.com/embed/sfp5KXNkqp0?rel=0&autoplay=1 VideoUrl_07681EF2_06F8_B474_419B_CAA0C566E454.url = //www.youtube.com/embed/sfp5KXNkqp0?rel=0&autoplay=1 VideoUrl_07681EF2_06F8_B474_4190_E2B23E4AA906.url = //www.youtube.com/embed/sfp5KXNkqp0?rel=0&autoplay=1 VideoUrl_2C13038F_A41F_97FE_41C9_8AB7B1626EDE.url = //www.youtube.com/embed/t2_9Mu7QywQ?rel=0&autoplay=1 VideoUrl_2C13038F_A41F_97FE_41C9_8AB7B1626EDE.url = //www.youtube.com/embed/t2_9Mu7QywQ?rel=0&autoplay=1 PopupWebFrameBehaviour_01C1975E_00D1_65D4_4158_C78336D77894.url = //www.youtube.com/embed/y2aRIX_CEnI?rel=0&autoplay=1 PopupWebFrameBehaviour_BACEB519_A993_5BED_41E3_C2F4DAA8D8D4.url = //www.youtube.com/embed/yCkpdAiUVRY?rel=0&autoplay=1 PopupWebFrameBehaviour_CE3A10FE_AA9D_BA27_41C8_86FEA41246D6.url = //www.youtube.com/embed/yGUtyolthAw?rel=0&autoplay=1 PopupWebFrameBehaviour_CB57308F_AA9D_BAE5_41E0_8DCF6A041AC3.url = //www.youtube.com/embed/yGUtyolthAw?rel=0&autoplay=1 PopupWebFrameBehaviour_EA89F1E7_A96C_DA25_41CD_455CE5C281FF.url = //www.youtube.com/embed/yacQ3mbhYlE?rel=0&autoplay=1 ## E-Learning ### Answer questionOption_C0B4860A_A406_B0E6_41D7_0EEB537F2C92.text = 0 degrees questionOption_C0B4860A_A406_B0E6_41D7_0EEB537F2C92.text = 0 degrees questionOption_C3A281D9_A402_9362_41D8_948DC2506A00.text = 029 questionOption_EB9CAF13_AAAC_E7FD_41E4_8CD80FFFD808.text = 030 or 210 questionOption_EB9F3F12_AAAC_E7FF_41E4_BA3397DFE160.text = 080 or 260 questionOption_2CE43D5D_C4F4_6894_4143_AA37DDBF2169.text = 1-2 m across questionOption_AC5841F3_C56F_54B9_41D1_7B6EF7F71C73.text = 10% questionOption_D944D89F_A41F_B11E_41DD_75469C3BB8C3.text = 15 degrees questionOption_D944D89F_A41F_B11E_41DD_75469C3BB8C3.text = 15 degrees questionOption_EB890F10_AAAC_E7FB_41D5_F75607F5EB7E.text = 156 or 336 questionOption_C3E00E2B_A40D_7125_41C1_43B08AED2C37.text = 180 questionOption_D45C4711_B990_7C85_41D4_1DF2BD986D6A.text = 2 cm questionOption_AC5F31F2_C56F_54BB_41E8_18B93D19B87A.text = 2% questionOption_D45D6713_B990_7C84_41E3_D27951CE4B4B.text = 20 cm questionOption_F84F174C_A405_BF62_41E2_03E51A78BC5F.text = 20 degrees northeast questionOption_F84F174C_A405_BF62_41E2_03E51A78BC5F.text = 20 degrees northeast questionOption_F808EAC9_A405_F162_41DB_87D33844A7FF.text = 20 degrees southwest questionOption_F808EAC9_A405_F162_41DB_87D33844A7FF.text = 20 degrees southwest questionOption_C35B02CD_A402_9162_41C8_C4E5325600A0.text = 220 questionOption_EB9DDF15_AAAC_E7E5_41DD_5B0537C528BC.text = 220 or 040 questionOption_2CE4BD5C_C4F4_6894_41E2_38337CB45296.text = 30-60 cm across questionOption_C8C1C556_A405_F36E_41D5_AF6AF20E95AE.text = 33 degrees NE questionOption_C8C1C556_A405_F36E_41D5_AF6AF20E95AE.text = 33 degrees NE questionOption_C3786437_A402_F12E_41C5_EBC990ACB0A0.text = 330 questionOption_CF6153AD_A402_9722_41E1_D7DE68DE9AF9.text = 43 degrees NE questionOption_CF6153AD_A402_9722_41E1_D7DE68DE9AF9.text = 43 degrees NE questionOption_D9F5BA13_A41F_F0E6_41B9_D420442C584C.text = 50 degrees questionOption_D9F5BA13_A41F_F0E6_41B9_D420442C584C.text = 50 degrees questionOption_C852BDBB_A405_9325_41A2_6BCF4926B39F.text = 50 degrees NE questionOption_C852BDBB_A405_9325_41A2_6BCF4926B39F.text = 50 degrees NE questionOption_AC5811F4_C56F_54BF_41DB_D2CAD0FFF9B3.text = 60% questionOption_D45DD712_B990_7C87_41E5_9FFEBA0EF809.text = 7 cm questionOption_F9CED9DE_A405_931E_41CB_BA3566C64F74.text = 80 degrees northwest questionOption_F9CED9DE_A405_931E_41CB_BA3566C64F74.text = 80 degrees northwest questionOption_F9886EBA_A406_9126_41C3_6709EA33416E.text = 87 degrees northeast questionOption_F9886EBA_A406_9126_41C3_6709EA33416E.text = 87 degrees northeast questionOption_D9BEF6A7_A41F_B12E_41D8_BB51C7596E10.text = 90 degrees questionOption_D9BEF6A7_A41F_B12E_41D8_BB51C7596E10.text = 90 degrees questionOption_AC5971F5_C56F_54B9_41C0_D107A9EBEC0F.text = 90% questionOption_2CE4DD5B_C4F4_689C_41E8_235426069FFC.text = <30 cm across questionOption_DE4616B8_A41E_9122_41E1_92619682644F.text = >150 degrees questionOption_DE4616B8_A41E_9122_41E1_92619682644F.text = >150 degrees questionOption_2CE7ED5E_C4F4_6894_41DD_F71829AFB498.text = >2 m across questionOption_A5E1E5F2_CD94_7BAC_41DB_1C1E70480D16.text = Basalt forms a chilled margin of a pyroxenite intrusion questionOption_A5182261_CD94_98AC_41D9_0FCD9E1F751F.text = Basalt forms a chilled margin of a pyroxenite intrusion questionOption_A518D263_CD94_98AC_41B9_06B38072D336.text = Basalt lava flow was extruded over pyroxenite questionOption_A5E145F3_CD94_7BAC_41E4_1EEB80DE64A4.text = Basalt lava flow was extruded over pyroxenite questionOption_A5E0B5EF_CD94_7BB4_41B5_F824255AD8CD.text = Basalt, pyroxenite and gabbro are different parts of a differentiated flow questionOption_A5199262_CD94_98AC_41DE_09A82AB376C2.text = Basalt, pyroxenite and gabbro are different parts of a differentiated flow questionOption_1FCC0ABE_8030_E2D0_41C5_C1693D33DD28.text = Cubic questionOption_BF1A568D_B990_9D9D_41CA_3C48A1919714.text = E - W questionOption_8831DB10_C329_3577_41D9_657D2B4D0F5D.text = E - W questionOption_4BCB1084_AC06_B1E2_4196_7CB9338FCF46.text = E-W questionOption_E34DF91E_B9F0_B4BF_41D3_C825450EA3BE.text = E-W questionOption_E9D1D7A9_A405_BF22_41D9_925BD2892CA9.text = E-W questionOption_D879AA5D_A406_B162_41DD_64509B6EA61B.text = E-W questionOption_60A7D8BB_BB8F_9585_41E4_C735F5A8431C.text = E-W questionOption_4BCB1084_AC06_B1E2_4196_7CB9338FCF46.text = E-W questionOption_D862CE80_A407_91E2_41C2_416279FCD004.text = E-W questionOption_BF1A1E4D_B990_8C9D_41DE_D1193300AA6E.text = E-W questionOption_E9D1D7A9_A405_BF22_41D9_925BD2892CA9.text = E-W questionOption_D862CE80_A407_91E2_41C2_416279FCD004.text = E-W questionOption_E791F9E3_B9F0_F785_41E0_20357602E680.text = E-W questionOption_4B061141_BA19_830C_41B5_5ECA76695731.text = Fieldspar questionOption_4B061141_BA19_830C_41B5_5ECA76695731.text = Fieldspar questionOption_4CF84401_AC05_70E2_41DD_7B3E4BCA5B6D.text = MH14, MH15, MH20, MH55, MH56 questionOption_4CF84401_AC05_70E2_41DD_7B3E4BCA5B6D.text = MH14, MH15, MH20, MH55, MH56 questionOption_BE9FC447_B88F_FC8D_41C5_7E31C518E472.text = MH14, MH15, MH20, MH55, MH56 questionOption_BE9FC443_B88F_FC85_41DF_19A14099AE96.text = MH15, MH14, MH20, MH55, MH56 questionOption_4E2109DB_AC02_F366_41E1_C523602996D9.text = MH15, MH14, MH20, MH55, MH56 questionOption_4E2109DB_AC02_F366_41E1_C523602996D9.text = MH15, MH14, MH20, MH55, MH56 questionOption_A42456DD_CD95_F994_41E6_3BA5F6DD43C4.text = MH50 is relatively depleted in silica and total alkalis questionOption_DEA907A1_A407_9F22_41DE_A55EB4B79AB2.text = MH55 and MH56 have positive and negative Ti anomalies, respectively questionOption_DEA907A1_A407_9F22_41DE_A55EB4B79AB2.text = MH55 and MH56 have positive and negative Ti anomalies, respectively questionOption_D98691FE_A406_931E_41DD_B9D1234951CB.text = MH55 has MORB-like abundances of REE questionOption_D98691FE_A406_931E_41DD_B9D1234951CB.text = MH55 has MORB-like abundances of REE questionOption_DE3ED421_A407_F122_41CA_C930F88F9BBD.text = MH55 has a significantly higher Th abundance questionOption_DE3ED421_A407_F122_41CA_C930F88F9BBD.text = MH55 has a significantly higher Th abundance questionOption_DFDB999F_A406_931E_41D0_380FE4AF4B91.text = MH55 has significantly depleted HREE and a stronger negative NB+Ta anomaly questionOption_DFDB999F_A406_931E_41D0_380FE4AF4B91.text = MH55 has significantly depleted HREE and a stronger negative NB+Ta anomaly questionOption_BE9FC445_B88F_FC8D_41DB_2464A507C8DB.text = MH56, MH20, MH55, MH15, MH14 questionOption_4F4E879D_AC02_BFE2_41D8_6DCF04B2C550.text = MH56, MH20, MH55, MH15, MH14 questionOption_4F4E879D_AC02_BFE2_41D8_6DCF04B2C550.text = MH56, MH20, MH55, MH15, MH14 questionOption_BE9FC441_B88F_FC85_41BF_00665127F844.text = MH56, MH55, MH20, MH14, MH15 questionOption_7132B69C_AC7E_91E2_41DA_D5D28B8EDB3B.text = MH56, MH55, MH20, MH14, MH15 questionOption_7132B69C_AC7E_91E2_41DA_D5D28B8EDB3B.text = MH56, MH55, MH20, MH14, MH15 questionOption_A41B86DC_CD95_F994_41E2_166E1BC516A5.text = MH58 is significantly more enriched in total alkalis questionOption_A41B16DB_CD95_F99C_41B2_2D1A03F55E7E.text = MH58 is significantly more silicious questionOption_BF1A568A_B990_9D87_41C3_3704EFC147FF.text = N - S questionOption_88329B0E_C329_356B_417A_F07506658542.text = N - S questionOption_60A868B9_BB8F_9585_41CD_606AB47072B8.text = N-S questionOption_D8CD1443_A406_9166_41B5_7696344967EA.text = N-S questionOption_75A8794D_AC05_9362_41DA_B4C55DE5969F.text = N-S questionOption_BF1A1E4A_B990_8C87_41D0_6C2350AF40CB.text = N-S questionOption_75A8794D_AC05_9362_41DA_B4C55DE5969F.text = N-S questionOption_D8CD1443_A406_9166_41B5_7696344967EA.text = N-S questionOption_D9E0E5F6_A406_B32E_41C6_B0D41DA9BEE8.text = N-S questionOption_E34E891A_B9F0_B487_41D3_8BD298AE677C.text = N-S questionOption_E86282CF_A405_917E_41CA_6D0EE7F691DA.text = N-S questionOption_E86282CF_A405_917E_41CA_6D0EE7F691DA.text = N-S questionOption_E79199DD_B9F0_F7BD_41DF_DB7CE67BC390.text = N-S questionOption_BF1A568B_B990_9D85_41E3_AEB1BEAC0F99.text = NE - SW questionOption_88310B0F_C329_3569_41B2_DCD0313D03BC.text = NE - SW questionOption_BF1A1E4B_B990_8C85_41D1_488DA7C98F19.text = NE-SW questionOption_4A0730AC_AC05_7122_41E0_9BEF91DBEFF5.text = NE-SW questionOption_E34E891B_B9F0_B485_41C1_4A9516AC83ED.text = NE-SW questionOption_60A8C8B6_BB8F_958F_41D5_9EEAE6F87684.text = NE-SW questionOption_D8007A00_A407_70E2_41D8_A806B6697922.text = NE-SW questionOption_D8140D49_A406_9362_41B0_5A40B2C48DE7.text = NE-SW questionOption_E9ABDD49_A405_F362_41DA_D1E5F78260CB.text = NE-SW questionOption_D8140D49_A406_9362_41B0_5A40B2C48DE7.text = NE-SW questionOption_4A0730AC_AC05_7122_41E0_9BEF91DBEFF5.text = NE-SW questionOption_E790C9DF_B9F0_F7BD_41DA_4E1D01CC4B52.text = NE-SW questionOption_E9ABDD49_A405_F362_41DA_D1E5F78260CB.text = NE-SW questionOption_88303B11_C329_3579_41C5_55F2EBF7BA35.text = NW - SE questionOption_BF1A568F_B990_9D9D_41AC_4B5B68F6A72D.text = NW - SE questionOption_DBA27975_A407_9322_41DC_193E5C75CA9A.text = NW-SE questionOption_E98C3105_A405_90E2_41C8_0DED95754C36.text = NW-SE questionOption_48F32113_AC06_F0E6_41DC_13ED976B074F.text = NW-SE questionOption_E98C3105_A405_90E2_41C8_0DED95754C36.text = NW-SE questionOption_E790F9E1_B9F0_F785_41DB_35B4B911BBF7.text = NW-SE questionOption_DBA27975_A407_9322_41DC_193E5C75CA9A.text = NW-SE questionOption_48F32113_AC06_F0E6_41DC_13ED976B074F.text = NW-SE questionOption_DBC6C6EF_A406_B13E_41E3_02DA50691863.text = NW-SE questionOption_60A838B8_BB8F_9583_41E4_023444E44C0D.text = NW-SE questionOption_BF1A1E4F_B990_8C9D_41E5_D6E02270CB8F.text = NW-SE questionOption_E34F691D_B9F0_B4BD_41C1_D4904A0F9688.text = NW-SE questionOption_4C72C2A9_BA19_811C_41D6_7CA02BF5F8FE.text = Olivine questionOption_4C72C2A9_BA19_811C_41D6_7CA02BF5F8FE.text = Olivine questionOption_F4821413_A40F_70E6_41D2_7FD984BC9854.text = Pb/Pb questionOption_F4821413_A40F_70E6_41D2_7FD984BC9854.text = Pb/Pb questionOption_1FD33AC4_8030_E2B0_41C1_A5429EDFA772.text = Prismatic questionOption_4F87C928_BA16_831C_41DC_45339F2B7920.text = Pyrite questionOption_4F87C928_BA16_831C_41DC_45339F2B7920.text = Pyrite questionOption_A5E015F1_CD94_7BAC_41D9_54804FDAC6FA.text = Pyroxenite and gabbro and intruded an earlier basalt flow questionOption_A5185260_CD94_98AC_41D2_6A3DBE83DD1D.text = Pyroxenite and gabbro and intruded an earlier basalt flow questionOption_4EC9C7F1_BA16_8F0C_41CC_61CA3C4ECDEE.text = Quartz questionOption_4EC9C7F1_BA16_8F0C_41CC_61CA3C4ECDEE.text = Quartz questionOption_1BB80470_9EC6_8540_41D5_28F4C3E04DC3.text = Sigma 1 =vertical, sigma 2 and 3 = horizontal questionOption_1BB9E473_9EC6_8540_41CB_F287E7B8F969.text = Sigma 2 = vertical, sigma 1 and 3 = horizontal questionOption_EAFE2284_A41B_5850_41D1_9C6AB6F59E70.text = Sigma 3 = ESE-WNW questionOption_EA8B8286_A41B_5850_41BA_69FB56BD932E.text = Sigma 3 = NNE-SSW questionOption_EA8A5287_A41B_5850_41C7_998AFF9138D5.text = Sigma 3 = vertical questionOption_1BB91475_9EC6_8540_41E3_DF531E994D80.text = Sigma 3 = vertical, sigma 1 and 2 = horizontal questionOption_1FD20AC2_8030_E2B0_41C4_2AC4E78E51D8.text = Spherical questionOption_BEE2D261_B8B1_9485_41E4_642A606FCA58.text = Striking E-W, dipping steeply N questionOption_BEE2D25F_B8B1_94BD_41E1_71D8E1B9AFD8.text = Striking E-W, dipping steeply N questionOption_BEE2D262_B8B1_9487_41E0_60B40833CECE.text = Striking N-S, dipping steeply E questionOption_BEE2D260_B8B1_9483_41E6_4723F9B70A0E.text = Striking N-S, dipping steeply W questionOption_1FD37AC0_8030_E2B0_41B3_566E26EA16CE.text = Tetrahedral questionOption_A424C6DA_CD95_F99C_41CE_7647BF76C28E.text = They are not significantly distinguishable questionOption_EB426850_A40F_9163_41BF_0FAD5E34A000.text = U/Pb questionOption_EB426850_A40F_9163_41BF_0FAD5E34A000.text = U/Pb questionOption_1609DDAD_AC05_9322_41D7_8F318423D4BD.text = a back-arc basin questionOption_1609DDAD_AC05_9322_41D7_8F318423D4BD.text = a back-arc basin questionOption_C1C1982C_AA93_EA2B_41A7_79F6EB5473D8.text = a dyke questionOption_C1C1082B_AA93_EA2D_41E3_4138EE3AC95B.text = a fault questionOption_C1C0F824_AA93_E9DB_41E2_04D061960105.text = a fold questionOption_11F7E7E3_AC02_BF26_41DA_5E934EF216D8.text = a mid-ocean ridge at a divergent plate boundary questionOption_11F7E7E3_AC02_BF26_41DA_5E934EF216D8.text = a mid-ocean ridge at a divergent plate boundary questionOption_04EF17BA_AC03_9F26_41D5_AD418092F2D3.text = actinolite questionOption_04EF17BA_AC03_9F26_41D5_AD418092F2D3.text = actinolite questionOption_1833C052_AC3D_9166_41BD_E3C454B95DB3.text = actinolite questionOption_1833C052_AC3D_9166_41BD_E3C454B95DB3.text = actinolite questionOption_1833C052_AC3D_9166_41BD_E3C454B95DB3.text = actinolite questionOption_1833C052_AC3D_9166_41BD_E3C454B95DB3.text = actinolite questionOption_0ABC0940_A1C2_8F40_41D4_A0D1DD8924D5.text = alkaline questionOption_EB90B616_C329_3F7B_41E5_38DA0186595E.text = all of the above questionOption_376E3019_A402_90E2_41B4_2A5F688270A5.text = amygdales – vesicles that have been later cemented by calcite questionOption_376E3019_A402_90E2_41B4_2A5F688270A5.text = amygdales – vesicles that have been later cemented by calcite questionOption_376E3019_A402_90E2_41B4_2A5F688270A5.text = amygdales – vesicles that have been later cemented by calcite questionOption_376E3019_A402_90E2_41B4_2A5F688270A5.text = amygdales – vesicles that have been later cemented by calcite questionOption_376E3019_A402_90E2_41B4_2A5F688270A5.text = amygdales – vesicles that have been later cemented by calcite questionOption_376E3019_A402_90E2_41B4_2A5F688270A5.text = amygdales – vesicles that have been later cemented by calcite questionOption_376E3019_A402_90E2_41B4_2A5F688270A5.text = amygdales – vesicles that have been later cemented by calcite questionOption_376E3019_A402_90E2_41B4_2A5F688270A5.text = amygdales – vesicles that have been later cemented by calcite questionOption_DC5A6F92_A403_6FE6_41C2_1CA13D38B70B.text = amygdaloidal questionOption_DC5A6F92_A403_6FE6_41C2_1CA13D38B70B.text = amygdaloidal questionOption_DC5A6F92_A403_6FE6_41C2_1CA13D38B70B.text = amygdaloidal questionOption_D2B3B4AB_A40E_F126_41E3_C92E9F396164.text = amygdaloidal questionOption_DC5A6F92_A403_6FE6_41C2_1CA13D38B70B.text = amygdaloidal questionOption_D2B3B4AB_A40E_F126_41E3_C92E9F396164.text = amygdaloidal questionOption_D2B3B4AB_A40E_F126_41E3_C92E9F396164.text = amygdaloidal questionOption_D2B3B4AB_A40E_F126_41E3_C92E9F396164.text = amygdaloidal questionOption_6172C5EF_BB8F_9F9D_41DC_A1CAA775DC98.text = amygdaloidal questionOption_D96636A5_A40D_9122_41DA_C1EAE6C5F71B.text = amygdaloidal basalt questionOption_D96636A5_A40D_9122_41DA_C1EAE6C5F71B.text = amygdaloidal basalt questionOption_E04AAD5F_A40E_931E_41D1_B5DAFD2A32B2.text = assimilation of continental crust questionOption_E04AAD5F_A40E_931E_41D1_B5DAFD2A32B2.text = assimilation of continental crust questionOption_E04AAD5F_A40E_931E_41D1_B5DAFD2A32B2.text = assimilation of continental crust questionOption_E04AAD5F_A40E_931E_41D1_B5DAFD2A32B2.text = assimilation of continental crust questionOption_E04AAD5F_A40E_931E_41D1_B5DAFD2A32B2.text = assimilation of continental crust questionOption_E04AAD5F_A40E_931E_41D1_B5DAFD2A32B2.text = assimilation of continental crust questionOption_E04AAD5F_A40E_931E_41D1_B5DAFD2A32B2.text = assimilation of continental crust questionOption_E04AAD5F_A40E_931E_41D1_B5DAFD2A32B2.text = assimilation of continental crust questionOption_BF090353_B970_7485_41E1_A32E1F8113F7.text = banded questionOption_01AA5EAA_AC0E_9126_41DC_CDAA11BC4928.text = basalt questionOption_6301CB8F_BB90_8B9D_41E3_E1AF42B0C64F.text = basalt questionOption_01AA5EAA_AC0E_9126_41DC_CDAA11BC4928.text = basalt questionOption_01AA5EAA_AC0E_9126_41DC_CDAA11BC4928.text = basalt questionOption_62A71AEF_BB91_959D_41BF_675CC860FD0F.text = basalt questionOption_AE6BB8FE_B890_957F_41DE_50A0FC6889DF.text = basalt questionOption_A2FD0D05_CD94_A874_41E4_B14D71FA76E0.text = basalt questionOption_01AA5EAA_AC0E_9126_41DC_CDAA11BC4928.text = basalt questionOption_BF090355_B970_748D_41E7_1A9D6BEB168B.text = bedded questionOption_A451359B_CD95_9B9C_41A4_02647451CF47.text = bladed, acicular questionOption_C5B52D5E_A40E_B31E_41D2_3916B24A19BE.text = blue symbol questionOption_FED4E51E_A40D_731E_41D3_2B543B5FB296.text = blue symbol questionOption_C5B52D5E_A40E_B31E_41D2_3916B24A19BE.text = blue symbol questionOption_FED4E51E_A40D_731E_41D3_2B543B5FB296.text = blue symbol questionOption_E470CC4C_B9F1_8C83_41A6_E52211BAC606.text = blue symbol questionOption_DD362E21_C3E9_2F59_41E2_9CA2DB931361.text = box folds questionOption_DD473C97_C3E9_7379_41E2_26597D07BE90.text = check historical records with the shire and/or Department of Mines Industry Regulation and safety questionOption_DD373E1F_C3E9_2F69_41BD_45B9BE2BE640.text = chevron questionOption_04518A6C_AC03_9123_41CE_2975C0AC9F42.text = chlorite questionOption_04518A6C_AC03_9123_41CE_2975C0AC9F42.text = chlorite questionOption_1BB013AA_AC3D_9727_41D3_0EFEFB328B9A.text = chlorite questionOption_1BB013AA_AC3D_9727_41D3_0EFEFB328B9A.text = chlorite questionOption_1BB013AA_AC3D_9727_41D3_0EFEFB328B9A.text = chlorite questionOption_1BB013AA_AC3D_9727_41D3_0EFEFB328B9A.text = chlorite questionOption_E4D2750F_A402_B0FE_41B3_2D4DCA11E3FC.text = chondritic questionOption_E4D2750F_A402_B0FE_41B3_2D4DCA11E3FC.text = chondritic questionOption_04303B1A_AC02_90E6_41C5_1C44400423A3.text = clinopyroxene questionOption_D74CDE3B_A405_F126_41C6_1A55A3155708.text = clinopyroxene questionOption_21F815F7_B88F_9F8D_41DB_D3AF017F7104.text = clinopyroxene questionOption_FB05075A_EC02_C9EB_41D5_2E9B7DB05485.text = clinopyroxene questionOption_D4C22B96_A402_97EE_41E2_E255BB12F99C.text = clinopyroxene questionOption_04303B1A_AC02_90E6_41C5_1C44400423A3.text = clinopyroxene questionOption_D4C22B96_A402_97EE_41E2_E255BB12F99C.text = clinopyroxene questionOption_D22F7F0E_A40D_90FE_41D3_30DC73E45B85.text = close questionOption_D22F7F0E_A40D_90FE_41D3_30DC73E45B85.text = close questionOption_DF47D25B_A405_7166_41E2_E6A9259580DE.text = close questionOption_DF47D25B_A405_7166_41E2_E6A9259580DE.text = close questionOption_D22F7F0E_A40D_90FE_41D3_30DC73E45B85.text = close questionOption_DF47D25B_A405_7166_41E2_E6A9259580DE.text = close questionOption_D22F7F0E_A40D_90FE_41D3_30DC73E45B85.text = close questionOption_DF47D25B_A405_7166_41E2_E6A9259580DE.text = close questionOption_D22F7F0E_A40D_90FE_41D3_30DC73E45B85.text = close questionOption_D22F7F0E_A40D_90FE_41D3_30DC73E45B85.text = close questionOption_D22F7F0E_A40D_90FE_41D3_30DC73E45B85.text = close questionOption_D22F7F0E_A40D_90FE_41D3_30DC73E45B85.text = close questionOption_18EBF8E4_AC03_B122_41D8_4A280CE9A30A.text = coarse grained questionOption_18EBF8E4_AC03_B122_41D8_4A280CE9A30A.text = coarse grained questionOption_0C8A2BA5_A1C2_83C0_41E3_8337429D325A.text = common Pb, Pb loss and inherited grains questionOption_C5470744_B991_BC83_41D4_CB4A2E5FE704.text = compaction due to burial questionOption_ACC253B4_C56E_D4BF_41DC_22B026087B18.text = concentric domains with microscopic spinifex texture questionOption_2BC41893_A406_91E6_41CB_A7377DC3460E.text = concentric shells of crystals questionOption_2BC41893_A406_91E6_41CB_A7377DC3460E.text = concentric shells of crystals questionOption_2BC41893_A406_91E6_41CB_A7377DC3460E.text = concentric shells of crystals questionOption_2BC41893_A406_91E6_41CB_A7377DC3460E.text = concentric shells of crystals questionOption_0581FF43_AC06_AF66_41D3_A5A00342647F.text = conchoidal questionOption_0581FF43_AC06_AF66_41D3_A5A00342647F.text = conchoidal questionOption_285B8373_A406_B726_41C9_24726328AE87.text = contamination by assimilation of silicious sediments into the magma questionOption_285B8373_A406_B726_41C9_24726328AE87.text = contamination by assimilation of silicious sediments into the magma questionOption_9B3D8057_A402_F16E_41D7_744C5ADF46C7.text = continuous and sheared questionOption_9B3D8057_A402_F16E_41D7_744C5ADF46C7.text = continuous and sheared questionOption_FFB4416D_A40F_9322_41E4_420FEE3300C7.text = cross bedded questionOption_C495C099_A403_B1E2_41D1_1FD1DDF443AC.text = cross bedded questionOption_C495C099_A403_B1E2_41D1_1FD1DDF443AC.text = cross bedded questionOption_FFB4416D_A40F_9322_41E4_420FEE3300C7.text = cross bedded questionOption_C0B03514_AB6D_FBFB_41B1_000ECBF67817.text = cross bedding questionOption_E0CA6ED6_A40D_B16E_41D5_6411861C83E0.text = cumulate questionOption_A5982153_CD95_B8EC_41DE_6E78C407E896.text = cumulate questionOption_E0CA6ED6_A40D_B16E_41D5_6411861C83E0.text = cumulate questionOption_E0CA6ED6_A40D_B16E_41D5_6411861C83E0.text = cumulate questionOption_E0CA6ED6_A40D_B16E_41D5_6411861C83E0.text = cumulate questionOption_E0CA6ED6_A40D_B16E_41D5_6411861C83E0.text = cumulate questionOption_E0CA6ED6_A40D_B16E_41D5_6411861C83E0.text = cumulate questionOption_E0CA6ED6_A40D_B16E_41D5_6411861C83E0.text = cumulate questionOption_E0CA6ED6_A40D_B16E_41D5_6411861C83E0.text = cumulate questionOption_A2FC3D03_CD94_A86C_41D7_3F9737194946.text = dacite questionOption_A3CCDEC2_C56F_2CDB_41E2_5F34AD665E3D.text = dark green, laminated questionOption_C5470747_B991_BC8D_41C3_8A6551F2CE74.text = deformation in a hot volcanic flow questionOption_A452B59E_CD95_9B94_41DF_08B43A602BAD.text = dendritic questionOption_31CC65A3_A403_7326_41E1_D7D7FDE96687.text = devitrification of volcanic glass – alteration of unstable glass by the growth of crystals questionOption_31CC65A3_A403_7326_41E1_D7D7FDE96687.text = devitrification of volcanic glass – alteration of unstable glass by the growth of crystals questionOption_31CC65A3_A403_7326_41E1_D7D7FDE96687.text = devitrification of volcanic glass – alteration of unstable glass by the growth of crystals questionOption_31CC65A3_A403_7326_41E1_D7D7FDE96687.text = devitrification of volcanic glass – alteration of unstable glass by the growth of crystals questionOption_31CC65A3_A403_7326_41E1_D7D7FDE96687.text = devitrification of volcanic glass – alteration of unstable glass by the growth of crystals questionOption_31CC65A3_A403_7326_41E1_D7D7FDE96687.text = devitrification of volcanic glass – alteration of unstable glass by the growth of crystals questionOption_31CC65A3_A403_7326_41E1_D7D7FDE96687.text = devitrification of volcanic glass – alteration of unstable glass by the growth of crystals questionOption_31CC65A3_A403_7326_41E1_D7D7FDE96687.text = devitrification of volcanic glass – alteration of unstable glass by the growth of crystals questionOption_EA8BE518_A41B_3870_41BC_C40F5E3A2495.text = discontinuous and echelon tip zones questionOption_3529AE20_A47E_B122_41C2_02140F35736F.text = discrete and sharp questionOption_3529AE20_A47E_B122_41C2_02140F35736F.text = discrete and sharp questionOption_D0F87C1D_A406_90E2_41B8_90610F36B5D8.text = dolerite questionOption_06C132BB_AC0F_9126_41DB_DD4166DA46A4.text = dolerite questionOption_06C132BB_AC0F_9126_41DB_DD4166DA46A4.text = dolerite questionOption_D0F87C1D_A406_90E2_41B8_90610F36B5D8.text = dolerite questionOption_06C132BB_AC0F_9126_41DB_DD4166DA46A4.text = dolerite questionOption_06C132BB_AC0F_9126_41DB_DD4166DA46A4.text = dolerite questionOption_D0F87C1D_A406_90E2_41B8_90610F36B5D8.text = dolerite questionOption_D0F87C1D_A406_90E2_41B8_90610F36B5D8.text = dolerite questionOption_62A48AF2_BB91_9587_41E0_5A7695953F76.text = dolerite questionOption_D0F87C1D_A406_90E2_41B8_90610F36B5D8.text = dolerite questionOption_D0F87C1D_A406_90E2_41B8_90610F36B5D8.text = dolerite questionOption_D0F87C1D_A406_90E2_41B8_90610F36B5D8.text = dolerite questionOption_63006B92_BB90_8B87_41CC_F210684DB210.text = dolerite questionOption_A2FC7D04_CD94_A874_41E9_1AB3D6681E3C.text = dolerite questionOption_D0F87C1D_A406_90E2_41B8_90610F36B5D8.text = dolerite questionOption_DC394039_A406_F122_41A9_77C1C92E5F0B.text = drift questionOption_DC394039_A406_F122_41A9_77C1C92E5F0B.text = drift questionOption_ACC2E3B5_C56E_D4B9_41E4_0DE1132995CF.text = drusy cement infill questionOption_A2BC40E2_CD94_99AC_41CE_2C8F8588F6EF.text = dunite questionOption_295A9D7E_C4F4_A894_41E1_F049D44AF3CD.text = enriched mid-ocean ridge basalt (E-MORB) with a component of assimilation of felsic Archaean crust questionOption_FB9643F6_A403_B72E_41B7_922CF71207F8.text = erosion in a fluvial environment questionOption_FB9643F6_A403_B72E_41B7_922CF71207F8.text = erosion in a fluvial environment questionOption_C1C17829_AA93_EA2D_41C6_74553005A8B1.text = erosive channel questionOption_2E835C24_C4F7_A8B4_41DE_ADA14799B7C0.text = explosive eruption of lava as a hot ash flow questionOption_0051DA5D_AC05_7162_41B2_DEC17996809D.text = extrusion into an aqueous body questionOption_0051DA5D_AC05_7162_41B2_DEC17996809D.text = extrusion into an aqueous body questionOption_2E828C22_C4F7_A8AC_41E9_25A2D05A6B6D.text = extrusion of lava into water (subaqueous) questionOption_2E82BC23_C4F7_A8AC_41C5_08455FECFA6C.text = extrusion of lava over land (subaerial) questionOption_A282A35D_CD94_F894_41D5_516520EF1573.text = felsic questionOption_94ABB8CD_A994_EA65_41C0_164FF8800F75.text = felsic questionOption_1D5A3763_8030_A270_41D2_400474B7161C.text = felsic questionOption_AD67882F_C56E_F3A9_41C6_DCABC608F07B.text = felsic dykes questionOption_D093AD21_A406_9322_41C1_2FA0AC74BB18.text = felsic porphyry questionOption_D093AD21_A406_9322_41C1_2FA0AC74BB18.text = felsic porphyry questionOption_D093AD21_A406_9322_41C1_2FA0AC74BB18.text = felsic porphyry questionOption_D093AD21_A406_9322_41C1_2FA0AC74BB18.text = felsic porphyry questionOption_D093AD21_A406_9322_41C1_2FA0AC74BB18.text = felsic porphyry questionOption_D093AD21_A406_9322_41C1_2FA0AC74BB18.text = felsic porphyry questionOption_D093AD21_A406_9322_41C1_2FA0AC74BB18.text = felsic porphyry questionOption_D093AD21_A406_9322_41C1_2FA0AC74BB18.text = felsic porphyry questionOption_1BA9DE33_AC02_9126_41B4_17574A4E1E63.text = fine grained questionOption_1BA9DE33_AC02_9126_41B4_17574A4E1E63.text = fine grained questionOption_AE6A9901_B890_9485_41A7_1265CEDC9CBF.text = fine grained felsic questionOption_C405DB66_A402_972E_41CB_670C59334464.text = finely laminated questionOption_FF28888A_A40E_91E6_41D9_FD9552165761.text = finely laminated questionOption_C405DB66_A402_972E_41CB_670C59334464.text = finely laminated questionOption_FF28888A_A40E_91E6_41D9_FD9552165761.text = finely laminated questionOption_FB55580A_A403_F0E6_41C4_A1870FE315BE.text = flattening due to compaction in a hot volcanic ash flow questionOption_FB55580A_A403_F0E6_41C4_A1870FE315BE.text = flattening due to compaction in a hot volcanic ash flow questionOption_FBCEC2CB_A402_9166_41D7_1F92BCB7EAF1.text = flattening due to tectonic deformation questionOption_FBCEC2CB_A402_9166_41D7_1F92BCB7EAF1.text = flattening due to tectonic deformation questionOption_DEE3E537_A40E_B32E_419E_A464DE03F1F7.text = focus on mapping metamorphic mineral assemblages to establish isograds questionOption_DEE3E537_A40E_B32E_419E_A464DE03F1F7.text = focus on mapping metamorphic mineral assemblages to establish isograds questionOption_DE42388C_A40E_B1E2_41E2_05BD60C122C6.text = focus on mapping regolith and alluvial cover questionOption_DE42388C_A40E_B1E2_41E2_05BD60C122C6.text = focus on mapping regolith and alluvial cover questionOption_D98E9598_A40F_73E2_41B1_B170A1E0C49B.text = focus on mapping rock textures that indicate primary depositional environments questionOption_D98E9598_A40F_73E2_41B1_B170A1E0C49B.text = focus on mapping rock textures that indicate primary depositional environments questionOption_D935A2DF_A40F_F11E_41CE_BA81C7A1DA22.text = focus on mapping rock types, ductile and brittle structures, and alteration, especially near known old workings questionOption_D935A2DF_A40F_F11E_41CE_BA81C7A1DA22.text = focus on mapping rock types, ductile and brittle structures, and alteration, especially near known old workings questionOption_DFBFF213_A43D_F0E6_41D7_38DE2D494875.text = folding involved layer-parallel shearing questionOption_DFBFF213_A43D_F0E6_41D7_38DE2D494875.text = folding involved layer-parallel shearing questionOption_DC6F794F_A43D_937E_41DF_D7448216CC9A.text = folding was very rapid questionOption_DC6F794F_A43D_937E_41DF_D7448216CC9A.text = folding was very rapid questionOption_DFE844B1_A43D_7122_41D5_7ABA1716D4FD.text = folds formed in response to folding questionOption_DFE844B1_A43D_7122_41D5_7ABA1716D4FD.text = folds formed in response to folding questionOption_BF090357_B970_748D_41CB_B0AEA75C720C.text = foliated questionOption_E76617C3_A405_9F66_41B8_5F8DA41950C9.text = fractional crystallization questionOption_E01A31B5_A40D_7322_41E0_41EE38244627.text = fractional crystallization questionOption_E01A31B5_A40D_7322_41E0_41EE38244627.text = fractional crystallization questionOption_E76617C3_A405_9F66_41B8_5F8DA41950C9.text = fractional crystallization questionOption_E01A31B5_A40D_7322_41E0_41EE38244627.text = fractional crystallization questionOption_E76617C3_A405_9F66_41B8_5F8DA41950C9.text = fractional crystallization questionOption_E76617C3_A405_9F66_41B8_5F8DA41950C9.text = fractional crystallization questionOption_E01A31B5_A40D_7322_41E0_41EE38244627.text = fractional crystallization questionOption_E01A31B5_A40D_7322_41E0_41EE38244627.text = fractional crystallization questionOption_E01A31B5_A40D_7322_41E0_41EE38244627.text = fractional crystallization questionOption_E01A31B5_A40D_7322_41E0_41EE38244627.text = fractional crystallization questionOption_E01A31B5_A40D_7322_41E0_41EE38244627.text = fractional crystallization questionOption_2800455F_A407_731E_41B0_533B08FA5C30.text = fractional crystallization of mafic magma questionOption_2800455F_A407_731E_41B0_533B08FA5C30.text = fractional crystallization of mafic magma questionOption_071D8F63_AC0F_AF26_41A5_065BAA4E2E55.text = gabbro questionOption_071D8F63_AC0F_AF26_41A5_065BAA4E2E55.text = gabbro questionOption_071D8F63_AC0F_AF26_41A5_065BAA4E2E55.text = gabbro questionOption_071D8F63_AC0F_AF26_41A5_065BAA4E2E55.text = gabbro questionOption_A2BCF0E0_CD94_99AC_41E3_C4FA47866166.text = gabbro questionOption_AE6B48FD_B890_957D_41C8_1CB5F5779342.text = gabbro questionOption_DDF0F507_A40E_F0EE_41A6_C21AD9C9EBF7.text = garnet questionOption_DDF0F507_A40E_F0EE_41A6_C21AD9C9EBF7.text = garnet questionOption_DDF0F507_A40E_F0EE_41A6_C21AD9C9EBF7.text = garnet questionOption_DDF0F507_A40E_F0EE_41A6_C21AD9C9EBF7.text = garnet questionOption_DC54F066_A402_B12E_41DF_89138D3D41F6.text = gentle questionOption_258B8FFB_A40E_EF26_41BA_61D5888C4F25.text = gentle questionOption_258B8FFB_A40E_EF26_41BA_61D5888C4F25.text = gentle questionOption_258B8FFB_A40E_EF26_41BA_61D5888C4F25.text = gentle questionOption_258B8FFB_A40E_EF26_41BA_61D5888C4F25.text = gentle questionOption_258B8FFB_A40E_EF26_41BA_61D5888C4F25.text = gentle questionOption_DC54F066_A402_B12E_41DF_89138D3D41F6.text = gentle questionOption_DC54F066_A402_B12E_41DF_89138D3D41F6.text = gentle questionOption_258B8FFB_A40E_EF26_41BA_61D5888C4F25.text = gentle questionOption_258B8FFB_A40E_EF26_41BA_61D5888C4F25.text = gentle questionOption_258B8FFB_A40E_EF26_41BA_61D5888C4F25.text = gentle questionOption_DC54F066_A402_B12E_41DF_89138D3D41F6.text = gentle questionOption_BEE50F83_B8B0_8B85_41BF_45AB66DAEB9D.text = gently dipping E questionOption_D0C57AB2_A4FD_9126_41DF_1D99CEF08AD5.text = gently dipping E questionOption_D0C57AB2_A4FD_9126_41DF_1D99CEF08AD5.text = gently dipping E questionOption_DD10D29B_A406_91E6_41CE_AC5DFB626690.text = gently plunging questionOption_D3A31AD6_A402_F16E_41D5_4D69B00CFF75.text = gently plunging questionOption_DD10D29B_A406_91E6_41CE_AC5DFB626690.text = gently plunging questionOption_D3A31AD6_A402_F16E_41D5_4D69B00CFF75.text = gently plunging questionOption_D3A31AD6_A402_F16E_41D5_4D69B00CFF75.text = gently plunging questionOption_D3A31AD6_A402_F16E_41D5_4D69B00CFF75.text = gently plunging questionOption_DDF34241_A407_B162_41E1_BEBB0C88E903.text = gradational questionOption_EA80D53C_A41B_38B0_41AF_77CC81B098F1.text = gradational questionOption_DDF34241_A407_B162_41E1_BEBB0C88E903.text = gradational questionOption_C0B07513_AB6D_FBFD_41D9_C9115E4FF513.text = graded bedding questionOption_D1E36BDD_A407_9762_41D9_3523A7B1F350.text = granite questionOption_D1E36BDD_A407_9762_41D9_3523A7B1F350.text = granite questionOption_D1E36BDD_A407_9762_41D9_3523A7B1F350.text = granite questionOption_D1E36BDD_A407_9762_41D9_3523A7B1F350.text = granite questionOption_62A91AED_BB91_959D_41D4_6984BFE49D21.text = granite questionOption_D1E36BDD_A407_9762_41D9_3523A7B1F350.text = granite questionOption_D1E36BDD_A407_9762_41D9_3523A7B1F350.text = granite questionOption_63016B8E_BB90_8B9F_41DA_E14F4D057FE2.text = granite questionOption_D1E36BDD_A407_9762_41D9_3523A7B1F350.text = granite questionOption_D1E36BDD_A407_9762_41D9_3523A7B1F350.text = granite questionOption_D26DB600_A407_B0E2_41D1_FF80A683B109.text = granitic / felsic questionOption_D26DB600_A407_B0E2_41D1_FF80A683B109.text = granitic / felsic questionOption_D26DB600_A407_B0E2_41D1_FF80A683B109.text = granitic / felsic questionOption_D0E76DA8_A40D_F322_41BB_D7DE2C9C79AE.text = granitic / felsic questionOption_D0E76DA8_A40D_F322_41BB_D7DE2C9C79AE.text = granitic / felsic questionOption_D0E76DA8_A40D_F322_41BB_D7DE2C9C79AE.text = granitic / felsic questionOption_D26DB600_A407_B0E2_41D1_FF80A683B109.text = granitic / felsic questionOption_D26DB600_A407_B0E2_41D1_FF80A683B109.text = granitic / felsic questionOption_D26DB600_A407_B0E2_41D1_FF80A683B109.text = granitic / felsic questionOption_D26DB600_A407_B0E2_41D1_FF80A683B109.text = granitic / felsic questionOption_D26DB600_A407_B0E2_41D1_FF80A683B109.text = granitic / felsic questionOption_D0E76DA8_A40D_F322_41BB_D7DE2C9C79AE.text = granitic / felsic questionOption_A5995150_CD95_B8EC_41E8_96409664E9A9.text = graphic questionOption_029970BA_AC05_B126_41E1_A9306999B06C.text = hackled questionOption_029970BA_AC05_B126_41E1_A9306999B06C.text = hackled questionOption_E42958CD_A403_9162_41DA_2D56DD04CCA7.text = heavy-REE enriched questionOption_E42958CD_A403_9162_41DA_2D56DD04CCA7.text = heavy-REE enriched questionOption_1F68C32D_AC02_F722_4188_39C1869C2840.text = highly enriched LREE and depleted HREE questionOption_1F68C32D_AC02_F722_4188_39C1869C2840.text = highly enriched LREE and depleted HREE questionOption_D064B96D_A402_B322_41C6_842FAD4A91CC.text = horizontal questionOption_D064B96D_A402_B322_41C6_842FAD4A91CC.text = horizontal questionOption_DDDDB41D_A406_B0E2_41CF_161AAE92AD55.text = horizontal questionOption_DDDDB41D_A406_B0E2_41CF_161AAE92AD55.text = horizontal questionOption_D064B96D_A402_B322_41C6_842FAD4A91CC.text = horizontal questionOption_D064B96D_A402_B322_41C6_842FAD4A91CC.text = horizontal questionOption_D4BB3B96_A402_F7EE_41CA_84495C6677F3.text = hornblende questionOption_D4BB3B96_A402_F7EE_41CA_84495C6677F3.text = hornblende questionOption_58B4ED27_BBB1_8C8D_41E1_1215B96A84AA.text = hornblende questionOption_21F885F6_B88F_9F8F_41D2_D599E68B553A.text = hornblende questionOption_E47B3909_A40D_90E2_41E2_78D60C3CFAC4.text = hydrothermal alteration questionOption_E47B3909_A40D_90E2_41E2_78D60C3CFAC4.text = hydrothermal alteration questionOption_E47B3909_A40D_90E2_41E2_78D60C3CFAC4.text = hydrothermal alteration questionOption_E47B3909_A40D_90E2_41E2_78D60C3CFAC4.text = hydrothermal alteration questionOption_E47B3909_A40D_90E2_41E2_78D60C3CFAC4.text = hydrothermal alteration questionOption_E47B3909_A40D_90E2_41E2_78D60C3CFAC4.text = hydrothermal alteration questionOption_E47B3909_A40D_90E2_41E2_78D60C3CFAC4.text = hydrothermal alteration questionOption_E47B3909_A40D_90E2_41E2_78D60C3CFAC4.text = hydrothermal alteration questionOption_28323056_A407_B16E_41E3_66B85EBF5317.text = hydrothermal silicification questionOption_28323056_A407_B16E_41E3_66B85EBF5317.text = hydrothermal silicification questionOption_DDB1821A_A407_70E6_41C8_521589A94745.text = inferred questionOption_DDB1821A_A407_70E6_41C8_521589A94745.text = inferred questionOption_0C891BA8_A1C2_83C0_41CD_F0EDFBE2069F.text = inherited grains, Pb loss, and magmatic crystallization questionOption_D2B6279A_A407_7FE6_41D1_792456BEB222.text = intermediate questionOption_D2B6279A_A407_7FE6_41D1_792456BEB222.text = intermediate questionOption_D2B6279A_A407_7FE6_41D1_792456BEB222.text = intermediate questionOption_D2B6279A_A407_7FE6_41D1_792456BEB222.text = intermediate questionOption_D0CA336D_A40D_9722_41D8_EFDCC33B4EA0.text = intermediate questionOption_D0CA336D_A40D_9722_41D8_EFDCC33B4EA0.text = intermediate questionOption_D0CA336D_A40D_9722_41D8_EFDCC33B4EA0.text = intermediate questionOption_D2B6279A_A407_7FE6_41D1_792456BEB222.text = intermediate questionOption_D2B6279A_A407_7FE6_41D1_792456BEB222.text = intermediate questionOption_D2B6279A_A407_7FE6_41D1_792456BEB222.text = intermediate questionOption_D0CA336D_A40D_9722_41D8_EFDCC33B4EA0.text = intermediate questionOption_A282735E_CD94_F894_41E8_EC243D847CF6.text = intermediate questionOption_D2B6279A_A407_7FE6_41D1_792456BEB222.text = intermediate questionOption_D7BB0E25_A40D_7122_41A1_702415DDD758.text = interstitial questionOption_D7BB0E25_A40D_7122_41A1_702415DDD758.text = interstitial questionOption_021B5BA4_AC05_7722_41E2_5203E6348B8C.text = irregular questionOption_021B5BA4_AC05_7722_41E2_5203E6348B8C.text = irregular questionOption_3549DBC1_A47D_7762_41E1_BBFFEA403EF4.text = irregular and indistinct questionOption_3549DBC1_A47D_7762_41E1_BBFFEA403EF4.text = irregular and indistinct questionOption_49658C57_BB90_8C8D_41B0_C2FC9C7F2BE5.text = is a hyperbyssal intrusion questionOption_517611ED_BB90_B79D_41DD_EA9A9528384C.text = is a hyperbyssal intrusion questionOption_48BB6AA8_BB91_9583_41E2_E1B5910D1D23.text = is a hyperbyssal intrusion questionOption_4E4608ED_BB93_959D_41B7_53001695051E.text = is a hyperbyssal intrusion cooled very slowly questionOption_4A4D84D9_BB90_7D85_41B4_5EA4C9DEC1E7.text = is a hyperbyssal intrusion cooled very slowly questionOption_4A964996_BB91_978F_41D0_E343048498B1.text = is a hyperbyssal intrusion cooled very slowly questionOption_4B3B0A4D_BB91_B49D_415B_9AB36255638C.text = is a hyperbyssal intrusion cooled very slowly questionOption_4A4D44DC_BB90_7D83_41E3_FDDE84D5140A.text = is a hyperbyssal intrusion with a two-stage cooling history questionOption_4A97399A_BB91_9787_41DC_C1E666B73F00.text = is a hyperbyssal intrusion with a two-stage cooling history questionOption_4E7958EF_BB93_959D_41DB_F361885FA2CF.text = is a hyperbyssal intrusion with a two-stage cooling history questionOption_4B38CA50_BB91_B483_41CF_E268240CE421.text = is a hyperbyssal intrusion with a two-stage cooling history questionOption_0094C6BC_AC1D_7122_41AE_191CA54F8C6B.text = is the age of metamorphism of the dyke questionOption_0094C6BC_AC1D_7122_41AE_191CA54F8C6B.text = is the age of metamorphism of the dyke questionOption_0094C6BC_AC1D_7122_41AE_191CA54F8C6B.text = is the age of metamorphism of the dyke questionOption_0094C6BC_AC1D_7122_41AE_191CA54F8C6B.text = is the age of metamorphism of the dyke questionOption_06958B75_AC07_7722_41BC_41B511301578.text = is the age when the dyke was exposed at the land surface questionOption_06958B75_AC07_7722_41BC_41B511301578.text = is the age when the dyke was exposed at the land surface questionOption_06958B75_AC07_7722_41BC_41B511301578.text = is the age when the dyke was exposed at the land surface questionOption_06958B75_AC07_7722_41BC_41B511301578.text = is the age when the dyke was exposed at the land surface questionOption_07412FB0_AC07_6F22_41DF_DAF006B50B88.text = is the best estimate of magmatic crystallization of the dyke questionOption_07412FB0_AC07_6F22_41DF_DAF006B50B88.text = is the best estimate of magmatic crystallization of the dyke questionOption_07412FB0_AC07_6F22_41DF_DAF006B50B88.text = is the best estimate of magmatic crystallization of the dyke questionOption_07412FB0_AC07_6F22_41DF_DAF006B50B88.text = is the best estimate of magmatic crystallization of the dyke questionOption_9EC3F036_B970_F48F_41DB_50113AEABD4A.text = it is a sedimentary structure found only is aeolain (wind-blown) deposits questionOption_D3934B95_A403_97E2_41D3_38EAC6C72AD8.text = it is felsic to intermediate in composition questionOption_D3934B95_A403_97E2_41D3_38EAC6C72AD8.text = it is felsic to intermediate in composition questionOption_D32BCB6B_A402_F726_41CE_797FA8B67DF9.text = it is mafic in composition questionOption_D32BCB6B_A402_F726_41CE_797FA8B67DF9.text = it is mafic in composition questionOption_9EC3D035_B970_F48D_41E7_19510BA776A5.text = it is strictly a marine only environment questionOption_D3D87CE3_A402_B126_41D5_FD93772AF043.text = it is ultramafic in composition questionOption_D3D87CE3_A402_B126_41D5_FD93772AF043.text = it is ultramafic in composition questionOption_166CC345_8031_E3B0_41D6_B9F0BFBBBF10.text = left lateral (sinistral) questionOption_DD183238_A406_F122_41C9_46FFAE344BE4.text = mafic questionOption_D3033A3D_A402_911D_41C3_ACA171F3CC60.text = mafic questionOption_1D5B4762_8030_A270_41D3_FAB300D863E0.text = mafic questionOption_DD183238_A406_F122_41C9_46FFAE344BE4.text = mafic questionOption_DD183238_A406_F122_41C9_46FFAE344BE4.text = mafic questionOption_94A5A8CF_A994_EA65_41E1_7D01FF4994C8.text = mafic questionOption_DD183238_A406_F122_41C9_46FFAE344BE4.text = mafic questionOption_DD183238_A406_F122_41C9_46FFAE344BE4.text = mafic questionOption_DD183238_A406_F122_41C9_46FFAE344BE4.text = mafic questionOption_A282735F_CD94_F894_41DD_C4CF49584E0D.text = mafic questionOption_D3033A3D_A402_911D_41C3_ACA171F3CC60.text = mafic questionOption_DD183238_A406_F122_41C9_46FFAE344BE4.text = mafic questionOption_D3033A3D_A402_911D_41C3_ACA171F3CC60.text = mafic questionOption_DD183238_A406_F122_41C9_46FFAE344BE4.text = mafic questionOption_D3033A3D_A402_911D_41C3_ACA171F3CC60.text = mafic questionOption_AD67482E_C56E_F3AB_41D8_2D15A9E14D74.text = mafic rocks questionOption_288F8651_A406_9165_41D0_F89D260270C0.text = magma mixing with coexisting siliceous melts questionOption_288F8651_A406_9165_41D0_F89D260270C0.text = magma mixing with coexisting siliceous melts questionOption_0C899BA6_A1C2_83C0_41DE_C95070B15C58.text = magnetic crystallization, common Pb, and Pb loss questionOption_DD47AC98_C3E9_7377_41E6_FD53775F879D.text = make a detailed geological field map of the area to develop and test the hypotheses questionOption_C45623F5_A403_7722_41DB_CF0CF13808AC.text = massive questionOption_C0B0A516_AB6D_FBE7_41DA_DDCCB5EA367E.text = massive questionOption_FF7BECBB_A40E_9126_41E0_6541276330E1.text = massive questionOption_C45623F5_A403_7722_41DB_CF0CF13808AC.text = massive questionOption_FF7BECBB_A40E_9126_41E0_6541276330E1.text = massive questionOption_BF090354_B970_7483_41E6_A57B3BFEF217.text = massive questionOption_DF9597CE_A405_9F7E_41DF_C8BC4DE30E92.text = massive, crystalline, coarse grained questionOption_DF9597CE_A405_9F7E_41DF_C8BC4DE30E92.text = massive, crystalline, coarse grained questionOption_DF9597CE_A405_9F7E_41DF_C8BC4DE30E92.text = massive, crystalline, coarse grained questionOption_DF9597CE_A405_9F7E_41DF_C8BC4DE30E92.text = massive, crystalline, coarse grained questionOption_DF77CE31_A405_B122_41E3_5AA44BF7DCC3.text = massive, crystalline, fine grained, aphyric questionOption_DF77CE31_A405_B122_41E3_5AA44BF7DCC3.text = massive, crystalline, fine grained, aphyric questionOption_DF77CE31_A405_B122_41E3_5AA44BF7DCC3.text = massive, crystalline, fine grained, aphyric questionOption_DF77CE31_A405_B122_41E3_5AA44BF7DCC3.text = massive, crystalline, fine grained, aphyric questionOption_DF3B1CE9_A405_7122_41DB_19B969B351FD.text = massive, crystalline, medium grained questionOption_DF3B1CE9_A405_7122_41DB_19B969B351FD.text = massive, crystalline, medium grained questionOption_DF3B1CE9_A405_7122_41DB_19B969B351FD.text = massive, crystalline, medium grained questionOption_DF3B1CE9_A405_7122_41DB_19B969B351FD.text = massive, crystalline, medium grained questionOption_DE3E7DF7_A405_932E_41DB_80E5928EF3C9.text = massive, crystalline, medium grained, porphyritic questionOption_DE3E7DF7_A405_932E_41DB_80E5928EF3C9.text = massive, crystalline, medium grained, porphyritic questionOption_DE3E7DF7_A405_932E_41DB_80E5928EF3C9.text = massive, crystalline, medium grained, porphyritic questionOption_DE3E7DF7_A405_932E_41DB_80E5928EF3C9.text = massive, crystalline, medium grained, porphyritic questionOption_186269C5_AC03_7362_41DD_F800A0F9B654.text = medium grained questionOption_186269C5_AC03_7362_41DD_F800A0F9B654.text = medium grained questionOption_E699A03C_A405_9122_41C3_682C75194987.text = melt extracted from a garnet-bearing source region questionOption_E699A03C_A405_9122_41C3_682C75194987.text = melt extracted from a garnet-bearing source region questionOption_E699A03C_A405_9122_41C3_682C75194987.text = melt extracted from a garnet-bearing source region questionOption_E699A03C_A405_9122_41C3_682C75194987.text = melt extracted from a garnet-bearing source region questionOption_E6B0F021_A405_9122_41D7_6629B290F1F8.text = melting of the depleted mantle at shallow depths questionOption_E6B0F021_A405_9122_41D7_6629B290F1F8.text = melting of the depleted mantle at shallow depths questionOption_E6B0F021_A405_9122_41D7_6629B290F1F8.text = melting of the depleted mantle at shallow depths questionOption_E6B0F021_A405_9122_41D7_6629B290F1F8.text = melting of the depleted mantle at shallow depths questionOption_E73F478A_A402_9FE6_41BB_53925FD46ADA.text = mixing of two magmas questionOption_E73F478A_A402_9FE6_41BB_53925FD46ADA.text = mixing of two magmas questionOption_E73F478A_A402_9FE6_41BB_53925FD46ADA.text = mixing of two magmas questionOption_E73F478A_A402_9FE6_41BB_53925FD46ADA.text = mixing of two magmas questionOption_D346D358_A4FD_7762_4192_161151CD894F.text = moderately dipping ENE questionOption_D346D358_A4FD_7762_4192_161151CD894F.text = moderately dipping ENE questionOption_D913D2C8_A403_9162_41D5_3EB4E4231408.text = no questionOption_D913D2C8_A403_9162_41D5_3EB4E4231408.text = no questionOption_295A1D7F_C4F4_A894_41D1_3EBED5B6F254.text = normal mid-ocean ridge basalt (N-MORB) with a component of assimilation of felsic Archaean crust questionOption_DC712F89_A406_AFE2_41D7_5E7452A27A58.text = observed questionOption_DC712F89_A406_AFE2_41D7_5E7452A27A58.text = observed questionOption_29557D7D_C4F4_A894_41DC_7E7A0C595E77.text = ocean island basalt (OIB) with progressive fractional crystallisation questionOption_36E91C3F_A402_911E_41E0_7B76A56C1DEA.text = ocelli – spherulitic crystallization within a magma chamber questionOption_36E91C3F_A402_911E_41E0_7B76A56C1DEA.text = ocelli – spherulitic crystallization within a magma chamber questionOption_36E91C3F_A402_911E_41E0_7B76A56C1DEA.text = ocelli – spherulitic crystallization within a magma chamber questionOption_36E91C3F_A402_911E_41E0_7B76A56C1DEA.text = ocelli – spherulitic crystallization within a magma chamber questionOption_36E91C3F_A402_911E_41E0_7B76A56C1DEA.text = ocelli – spherulitic crystallization within a magma chamber questionOption_36E91C3F_A402_911E_41E0_7B76A56C1DEA.text = ocelli – spherulitic crystallization within a magma chamber questionOption_36E91C3F_A402_911E_41E0_7B76A56C1DEA.text = ocelli – spherulitic crystallization within a magma chamber questionOption_36E91C3F_A402_911E_41E0_7B76A56C1DEA.text = ocelli – spherulitic crystallization within a magma chamber questionOption_21F9E5F4_B88F_9F83_41E2_E3B85FC8325C.text = olivine questionOption_DA534401_A405_B0E2_41D5_76C2FF9EB360.text = olivine questionOption_DA534401_A405_B0E2_41D5_76C2FF9EB360.text = olivine questionOption_DCA285FC_A40F_9322_41D1_580821C7E799.text = olivine questionOption_DCA285FC_A40F_9322_41D1_580821C7E799.text = olivine questionOption_FA11DE4B_A405_B166_41D3_235CCCF324DC.text = olivine questionOption_DB47BCEB_A405_7126_41D4_87262F47C9E4.text = olivine questionOption_0F680FCA_BB90_8B87_41E3_1562E5FCC50D.text = olivine questionOption_DCA285FC_A40F_9322_41D1_580821C7E799.text = olivine questionOption_FA11DE4B_A405_B166_41D3_235CCCF324DC.text = olivine questionOption_FB056758_EC02_C9F7_41EA_C7191CD1CB4D.text = olivine questionOption_07936C7E_AC02_911E_41E2_CA544909B861.text = olivine questionOption_DCA285FC_A40F_9322_41D1_580821C7E799.text = olivine questionOption_07936C7E_AC02_911E_41E2_CA544909B861.text = olivine questionOption_D2DE9E17_A40E_B0EE_41C7_8C7B1FF5B7B9.text = open questionOption_D2DE9E17_A40E_B0EE_41C7_8C7B1FF5B7B9.text = open questionOption_DF38AF1F_A405_AF1D_41D1_E5D0E89A55CB.text = open questionOption_DF38AF1F_A405_AF1D_41D1_E5D0E89A55CB.text = open questionOption_D2DE9E17_A40E_B0EE_41C7_8C7B1FF5B7B9.text = open questionOption_D2DE9E17_A40E_B0EE_41C7_8C7B1FF5B7B9.text = open questionOption_D2DE9E17_A40E_B0EE_41C7_8C7B1FF5B7B9.text = open questionOption_D2DE9E17_A40E_B0EE_41C7_8C7B1FF5B7B9.text = open questionOption_D2DE9E17_A40E_B0EE_41C7_8C7B1FF5B7B9.text = open questionOption_DF38AF1F_A405_AF1D_41D1_E5D0E89A55CB.text = open questionOption_D2DE9E17_A40E_B0EE_41C7_8C7B1FF5B7B9.text = open questionOption_DF38AF1F_A405_AF1D_41D1_E5D0E89A55CB.text = open questionOption_D7D694CC_A40E_9163_41D8_0F2231F157B0.text = ophitic questionOption_617185F2_BB8F_9F87_41E6_9FBE6BA9FB69.text = ophitic questionOption_D7D694CC_A40E_9163_41D8_0F2231F157B0.text = ophitic questionOption_A5997151_CD95_B8EC_41C2_1ECAD9810804.text = ophitic questionOption_D732D853_A403_B166_41E0_75266BCDD6A9.text = orthopyroxene questionOption_D795A143_A405_9366_41D1_021F7DF4ECFD.text = orthopyroxene questionOption_FB06B75B_EC02_C9E9_41D4_7F99E4296B4E.text = orthopyroxene questionOption_0F68DFCC_BB90_8B83_41E6_CE8A6AD602A3.text = orthopyroxene questionOption_D732D853_A403_B166_41E0_75266BCDD6A9.text = orthopyroxene questionOption_58B41D2E_BBB1_8C9F_41DA_A467D04EE66C.text = orthopyroxene questionOption_21F795F8_B88F_9F83_41E4_C02A8D9A355C.text = orthopyroxene questionOption_A3CCCEC1_C56F_2CD9_41E2_89A5F2AA0D1A.text = pale green, laminated questionOption_A3CCEEBF_C56F_2CA9_41E8_4BB9DD0CD233.text = pale green, spotted questionOption_A3CDAEC3_C56F_2CD9_41C3_74A1C9445757.text = pale, green, massive questionOption_1974D3A7_AC03_F72E_4183_FED7A7F0B089.text = pegmatitic questionOption_1974D3A7_AC03_F72E_4183_FED7A7F0B089.text = pegmatitic questionOption_0765DB48_AC0F_7762_41DF_D7891D2CA193.text = pegmatitic gabbro questionOption_0765DB48_AC0F_7762_41DF_D7891D2CA193.text = pegmatitic gabbro questionOption_0765DB48_AC0F_7762_41DF_D7891D2CA193.text = pegmatitic gabbro questionOption_0765DB48_AC0F_7762_41DF_D7891D2CA193.text = pegmatitic gabbro questionOption_A2BC90DF_CD94_9994_41DC_E1D49FA20F46.text = peridotite questionOption_BF1A3ED6_B990_8D8F_4198_842BF9FF8661.text = pervasive schistosity questionOption_D78FA47F_A40E_911E_41DB_9D2A5D46D872.text = phenocryst questionOption_D78FA47F_A40E_911E_41DB_9D2A5D46D872.text = phenocryst questionOption_DDB28EE7_A40E_B12E_41BC_5ED5D773AE0A.text = plagioclase questionOption_58B37D2F_BBB1_8C9D_41CA_4A50434D2095.text = plagioclase questionOption_DDB28EE7_A40E_B12E_41BC_5ED5D773AE0A.text = plagioclase questionOption_DDB28EE7_A40E_B12E_41BC_5ED5D773AE0A.text = plagioclase questionOption_DDB28EE7_A40E_B12E_41BC_5ED5D773AE0A.text = plagioclase questionOption_1B3B2584_AC3D_93E2_41D3_D8EA236FEC08.text = plagioclase questionOption_FB051759_EC02_C9E9_41E9_F65160EBD64D.text = plagioclase questionOption_1B3B2584_AC3D_93E2_41D3_D8EA236FEC08.text = plagioclase questionOption_1B3B2584_AC3D_93E2_41D3_D8EA236FEC08.text = plagioclase questionOption_1B3B2584_AC3D_93E2_41D3_D8EA236FEC08.text = plagioclase questionOption_0F699FC9_BB90_8B85_41D2_5C4B0E8AA8E9.text = plagioclase questionOption_D77F7ED8_A405_B162_41AB_59FC2FDFC308.text = plagioclase questionOption_AD665830_C56E_F3B7_41BD_254D96FA9AB4.text = plagiogranite questionOption_C0BE4511_AB6D_FBFD_41DE_F1ED341AEBAF.text = planar laminations questionOption_176E62DC_AC05_F162_41D3_7CA322C32FFA.text = plume-related ocean island volcanism questionOption_176E62DC_AC05_F162_41D3_7CA322C32FFA.text = plume-related ocean island volcanism questionOption_DD913705_A40F_90E2_4190_30DC13E8FB3B.text = poikilitic questionOption_DF5DD54F_A402_937E_41B1_57263D106975.text = poikilitic questionOption_617135F4_BB8F_9F83_41E0_D52CD4673B08.text = poikilitic questionOption_DD913705_A40F_90E2_4190_30DC13E8FB3B.text = poikilitic questionOption_DF5DD54F_A402_937E_41B1_57263D106975.text = poikilitic questionOption_DD913705_A40F_90E2_4190_30DC13E8FB3B.text = poikilitic questionOption_DF5DD54F_A402_937E_41B1_57263D106975.text = poikilitic questionOption_D952AAB8_A40D_B122_41E2_B2B889F64A88.text = poikilitic questionOption_D952AAB8_A40D_B122_41E2_B2B889F64A88.text = poikilitic questionOption_DD913705_A40F_90E2_4190_30DC13E8FB3B.text = poikilitic questionOption_DF5DD54F_A402_937E_41B1_57263D106975.text = poikilitic questionOption_D9BF8403_A402_F0E6_41B2_7AD3C0D1C687.text = poikilitic basalt questionOption_D9BF8403_A402_F0E6_41B2_7AD3C0D1C687.text = poikilitic basalt questionOption_DD368E22_C3E9_2F5B_41B3_C4ABBF4E4CA9.text = polyharmonic questionOption_ACC3A3B6_C56E_D4BB_41E7_533D2135F5E2.text = pore space questionOption_D2DBCFF9_A40E_AF22_41CD_56C531A39246.text = porphyritic questionOption_DC37B57D_A402_9322_41C1_1C0EF7E0E8DE.text = porphyritic questionOption_D2DBCFF9_A40E_AF22_41CD_56C531A39246.text = porphyritic questionOption_DC37B57D_A402_9322_41C1_1C0EF7E0E8DE.text = porphyritic questionOption_D2DBCFF9_A40E_AF22_41CD_56C531A39246.text = porphyritic questionOption_DC37B57D_A402_9322_41C1_1C0EF7E0E8DE.text = porphyritic questionOption_D2DBCFF9_A40E_AF22_41CD_56C531A39246.text = porphyritic questionOption_DC37B57D_A402_9322_41C1_1C0EF7E0E8DE.text = porphyritic questionOption_A5999152_CD95_B8EC_41E0_1F377BF78CB6.text = porphyritic questionOption_D176F93B_A402_9326_41C3_DC041383766B.text = porphyritic andesite questionOption_D176F93B_A402_9326_41C3_DC041383766B.text = porphyritic andesite questionOption_D176F93B_A402_9326_41C3_DC041383766B.text = porphyritic andesite questionOption_D176F93B_A402_9326_41C3_DC041383766B.text = porphyritic andesite questionOption_D176F93B_A402_9326_41C3_DC041383766B.text = porphyritic andesite questionOption_D176F93B_A402_9326_41C3_DC041383766B.text = porphyritic andesite questionOption_D176F93B_A402_9326_41C3_DC041383766B.text = porphyritic andesite questionOption_D176F93B_A402_9326_41C3_DC041383766B.text = porphyritic andesite questionOption_D176F93B_A402_9326_41C3_DC041383766B.text = porphyritic andesite questionOption_D176F93B_A402_9326_41C3_DC041383766B.text = porphyritic andesite questionOption_D176F93B_A402_9326_41C3_DC041383766B.text = porphyritic andesite questionOption_D1C19918_A47F_F0E2_41E1_9E3FABE556EF.text = porphyritic andesite questionOption_D176F93B_A402_9326_41C3_DC041383766B.text = porphyritic andesite questionOption_D176F93B_A402_9326_41C3_DC041383766B.text = porphyritic andesite questionOption_D176F93B_A402_9326_41C3_DC041383766B.text = porphyritic andesite questionOption_D176F93B_A402_9326_41C3_DC041383766B.text = porphyritic andesite questionOption_D176F93B_A402_9326_41C3_DC041383766B.text = porphyritic andesite questionOption_D1C19918_A47F_F0E2_41E1_9E3FABE556EF.text = porphyritic andesite questionOption_D1C19918_A47F_F0E2_41E1_9E3FABE556EF.text = porphyritic andesite questionOption_D1C19918_A47F_F0E2_41E1_9E3FABE556EF.text = porphyritic andesite questionOption_D1C19918_A47F_F0E2_41E1_9E3FABE556EF.text = porphyritic andesite questionOption_D1C19918_A47F_F0E2_41E1_9E3FABE556EF.text = porphyritic andesite questionOption_D1C19918_A47F_F0E2_41E1_9E3FABE556EF.text = porphyritic andesite questionOption_D1C19918_A47F_F0E2_41E1_9E3FABE556EF.text = porphyritic andesite questionOption_D1F624CF_A41D_717E_41BB_71B7451980E5.text = porphyritic dolerite questionOption_D1F624CF_A41D_717E_41BB_71B7451980E5.text = porphyritic dolerite questionOption_D1F624CF_A41D_717E_41BB_71B7451980E5.text = porphyritic dolerite questionOption_D1F624CF_A41D_717E_41BB_71B7451980E5.text = porphyritic dolerite questionOption_D1F624CF_A41D_717E_41BB_71B7451980E5.text = porphyritic dolerite questionOption_D1F624CF_A41D_717E_41BB_71B7451980E5.text = porphyritic dolerite questionOption_D1F624CF_A41D_717E_41BB_71B7451980E5.text = porphyritic dolerite questionOption_D1F624CF_A41D_717E_41BB_71B7451980E5.text = porphyritic dolerite questionOption_D1F624CF_A41D_717E_41BB_71B7451980E5.text = porphyritic dolerite questionOption_D1F624CF_A41D_717E_41BB_71B7451980E5.text = porphyritic dolerite questionOption_D1F624CF_A41D_717E_41BB_71B7451980E5.text = porphyritic dolerite questionOption_D1F624CF_A41D_717E_41BB_71B7451980E5.text = porphyritic dolerite questionOption_D04BB86E_A47E_B13E_41E0_4D8BB4FB1268.text = porphyritic dolerite questionOption_D1F624CF_A41D_717E_41BB_71B7451980E5.text = porphyritic dolerite questionOption_D1F624CF_A41D_717E_41BB_71B7451980E5.text = porphyritic dolerite questionOption_D1F624CF_A41D_717E_41BB_71B7451980E5.text = porphyritic dolerite questionOption_D1F624CF_A41D_717E_41BB_71B7451980E5.text = porphyritic dolerite questionOption_D04BB86E_A47E_B13E_41E0_4D8BB4FB1268.text = porphyritic dolerite questionOption_D04BB86E_A47E_B13E_41E0_4D8BB4FB1268.text = porphyritic dolerite questionOption_D04BB86E_A47E_B13E_41E0_4D8BB4FB1268.text = porphyritic dolerite questionOption_D04BB86E_A47E_B13E_41E0_4D8BB4FB1268.text = porphyritic dolerite questionOption_D04BB86E_A47E_B13E_41E0_4D8BB4FB1268.text = porphyritic dolerite questionOption_D04BB86E_A47E_B13E_41E0_4D8BB4FB1268.text = porphyritic dolerite questionOption_D04BB86E_A47E_B13E_41E0_4D8BB4FB1268.text = porphyritic dolerite questionOption_D1830A4A_A402_9166_41BA_93DDDC68A0BF.text = porphyritic granite questionOption_D1830A4A_A402_9166_41BA_93DDDC68A0BF.text = porphyritic granite questionOption_D1830A4A_A402_9166_41BA_93DDDC68A0BF.text = porphyritic granite questionOption_D1830A4A_A402_9166_41BA_93DDDC68A0BF.text = porphyritic granite questionOption_D071F5A6_A47F_732E_41D1_3A83CC8B2F9F.text = porphyritic granite questionOption_D1830A4A_A402_9166_41BA_93DDDC68A0BF.text = porphyritic granite questionOption_D1830A4A_A402_9166_41BA_93DDDC68A0BF.text = porphyritic granite questionOption_D1830A4A_A402_9166_41BA_93DDDC68A0BF.text = porphyritic granite questionOption_D1830A4A_A402_9166_41BA_93DDDC68A0BF.text = porphyritic granite questionOption_D071F5A6_A47F_732E_41D1_3A83CC8B2F9F.text = porphyritic granite questionOption_D071F5A6_A47F_732E_41D1_3A83CC8B2F9F.text = porphyritic granite questionOption_D1830A4A_A402_9166_41BA_93DDDC68A0BF.text = porphyritic granite questionOption_D071F5A6_A47F_732E_41D1_3A83CC8B2F9F.text = porphyritic granite questionOption_D1830A4A_A402_9166_41BA_93DDDC68A0BF.text = porphyritic granite questionOption_D071F5A6_A47F_732E_41D1_3A83CC8B2F9F.text = porphyritic granite questionOption_D1830A4A_A402_9166_41BA_93DDDC68A0BF.text = porphyritic granite questionOption_D1830A4A_A402_9166_41BA_93DDDC68A0BF.text = porphyritic granite questionOption_D071F5A6_A47F_732E_41D1_3A83CC8B2F9F.text = porphyritic granite questionOption_D1830A4A_A402_9166_41BA_93DDDC68A0BF.text = porphyritic granite questionOption_D071F5A6_A47F_732E_41D1_3A83CC8B2F9F.text = porphyritic granite questionOption_D1830A4A_A402_9166_41BA_93DDDC68A0BF.text = porphyritic granite questionOption_D1830A4A_A402_9166_41BA_93DDDC68A0BF.text = porphyritic granite questionOption_D1830A4A_A402_9166_41BA_93DDDC68A0BF.text = porphyritic granite questionOption_D071F5A6_A47F_732E_41D1_3A83CC8B2F9F.text = porphyritic granite questionOption_D02949EF_A41D_B33E_41D1_7E255675D2EF.text = porphyritic pyroxenite questionOption_D02949EF_A41D_B33E_41D1_7E255675D2EF.text = porphyritic pyroxenite questionOption_D02949EF_A41D_B33E_41D1_7E255675D2EF.text = porphyritic pyroxenite questionOption_D02949EF_A41D_B33E_41D1_7E255675D2EF.text = porphyritic pyroxenite questionOption_D02949EF_A41D_B33E_41D1_7E255675D2EF.text = porphyritic pyroxenite questionOption_D02949EF_A41D_B33E_41D1_7E255675D2EF.text = porphyritic pyroxenite questionOption_D02949EF_A41D_B33E_41D1_7E255675D2EF.text = porphyritic pyroxenite questionOption_D02949EF_A41D_B33E_41D1_7E255675D2EF.text = porphyritic pyroxenite questionOption_D02949EF_A41D_B33E_41D1_7E255675D2EF.text = porphyritic pyroxenite questionOption_D02949EF_A41D_B33E_41D1_7E255675D2EF.text = porphyritic pyroxenite questionOption_D0A7AA8E_A47E_F1FE_41E1_69E6D0E1E3D3.text = porphyritic pyroxenite questionOption_D02949EF_A41D_B33E_41D1_7E255675D2EF.text = porphyritic pyroxenite questionOption_D0A7AA8E_A47E_F1FE_41E1_69E6D0E1E3D3.text = porphyritic pyroxenite questionOption_D02949EF_A41D_B33E_41D1_7E255675D2EF.text = porphyritic pyroxenite questionOption_D0A7AA8E_A47E_F1FE_41E1_69E6D0E1E3D3.text = porphyritic pyroxenite questionOption_D0A7AA8E_A47E_F1FE_41E1_69E6D0E1E3D3.text = porphyritic pyroxenite questionOption_D02949EF_A41D_B33E_41D1_7E255675D2EF.text = porphyritic pyroxenite questionOption_D0A7AA8E_A47E_F1FE_41E1_69E6D0E1E3D3.text = porphyritic pyroxenite questionOption_D0A7AA8E_A47E_F1FE_41E1_69E6D0E1E3D3.text = porphyritic pyroxenite questionOption_D0A7AA8E_A47E_F1FE_41E1_69E6D0E1E3D3.text = porphyritic pyroxenite questionOption_D02949EF_A41D_B33E_41D1_7E255675D2EF.text = porphyritic pyroxenite questionOption_D0A7AA8E_A47E_F1FE_41E1_69E6D0E1E3D3.text = porphyritic pyroxenite questionOption_D02949EF_A41D_B33E_41D1_7E255675D2EF.text = porphyritic pyroxenite questionOption_D02949EF_A41D_B33E_41D1_7E255675D2EF.text = porphyritic pyroxenite questionOption_DD378E20_C3E9_2F57_41B2_BD2CE38344AD.text = ptygmatic questionOption_FBD3E6FF_A402_911E_41D8_F288B0BBA4F0.text = pyrite questionOption_FBD3E6FF_A402_911E_41D8_F288B0BBA4F0.text = pyrite questionOption_FBAD8B33_A402_9726_41E0_5996DC5DF963.text = pyroxene questionOption_FBAD8B33_A402_9726_41E0_5996DC5DF963.text = pyroxene questionOption_A2BCF0E1_CD94_99AC_41DE_51C47834D5AC.text = pyroxene questionOption_D0B61C75_A406_9122_41DD_406DE86ECA40.text = pyroxenite questionOption_D0B61C75_A406_9122_41DD_406DE86ECA40.text = pyroxenite questionOption_D0B61C75_A406_9122_41DD_406DE86ECA40.text = pyroxenite questionOption_D0B61C75_A406_9122_41DD_406DE86ECA40.text = pyroxenite questionOption_D0B61C75_A406_9122_41DD_406DE86ECA40.text = pyroxenite questionOption_D0B61C75_A406_9122_41DD_406DE86ECA40.text = pyroxenite questionOption_D0B61C75_A406_9122_41DD_406DE86ECA40.text = pyroxenite questionOption_D0B61C75_A406_9122_41DD_406DE86ECA40.text = pyroxenite questionOption_FA452E0B_A405_90E6_41D8_97F3C7F4F35C.text = quartz questionOption_1A929804_AC02_90E2_41E0_9B3D5BD2D3DB.text = quartz questionOption_FA452E0B_A405_90E6_41D8_97F3C7F4F35C.text = quartz questionOption_0F69CFC7_BB90_8B8D_41C4_7E38D4072CA6.text = quartz questionOption_1A929804_AC02_90E2_41E0_9B3D5BD2D3DB.text = quartz questionOption_1A929804_AC02_90E2_41E0_9B3D5BD2D3DB.text = quartz questionOption_1A929804_AC02_90E2_41E0_9B3D5BD2D3DB.text = quartz questionOption_58B49D2D_BBB1_8C9D_41E6_4527796AA40E.text = quartz questionOption_3662F61E_A402_B11E_41D7_27F169C0F6B8.text = quenched droplets of immiscible liquid in a lava questionOption_3662F61E_A402_B11E_41D7_27F169C0F6B8.text = quenched droplets of immiscible liquid in a lava questionOption_3662F61E_A402_B11E_41D7_27F169C0F6B8.text = quenched droplets of immiscible liquid in a lava questionOption_3662F61E_A402_B11E_41D7_27F169C0F6B8.text = quenched droplets of immiscible liquid in a lava questionOption_3662F61E_A402_B11E_41D7_27F169C0F6B8.text = quenched droplets of immiscible liquid in a lava questionOption_3662F61E_A402_B11E_41D7_27F169C0F6B8.text = quenched droplets of immiscible liquid in a lava questionOption_3662F61E_A402_B11E_41D7_27F169C0F6B8.text = quenched droplets of immiscible liquid in a lava questionOption_3662F61E_A402_B11E_41D7_27F169C0F6B8.text = quenched droplets of immiscible liquid in a lava questionOption_280BC342_A406_9767_41A4_8FCACB428464.text = radiating crystals questionOption_280BC342_A406_9767_41A4_8FCACB428464.text = radiating crystals questionOption_280BC342_A406_9767_41A4_8FCACB428464.text = radiating crystals questionOption_280BC342_A406_9767_41A4_8FCACB428464.text = radiating crystals questionOption_03E8CA22_AC05_B126_419A_C8533DA77234.text = rapid quenching of a lava questionOption_03E8CA22_AC05_B126_419A_C8533DA77234.text = rapid quenching of a lava questionOption_DD471C9A_C3E9_736B_41DD_8FEA7B51A4E8.text = read academic literature on gold mineralization in the region questionOption_C5E8B94A_A40E_F366_41DF_6B76FED16916.text = red symbol questionOption_E47F6C4A_B9F1_8C87_41D5_AE54CC0597A3.text = red symbol questionOption_FD34BAF0_A40D_B123_41D6_5C98BE0035CA.text = red symbol questionOption_FD34BAF0_A40D_B123_41D6_5C98BE0035CA.text = red symbol questionOption_C5E8B94A_A40E_F366_41DF_6B76FED16916.text = red symbol questionOption_9EC34034_B970_F483_41D7_47EA7A507EDE.text = requires flow to form an erosive base questionOption_A2FCAD02_CD94_A86C_41E6_FD2CE97645FB.text = rhyolite questionOption_166F0344_8031_E3B0_41DC_2FD15A00B43A.text = right lateral (dextral) questionOption_DC078BDA_A40F_B766_41E1_893074B7AC0B.text = rutile questionOption_DC078BDA_A40F_B766_41E1_893074B7AC0B.text = rutile questionOption_DC078BDA_A40F_B766_41E1_893074B7AC0B.text = rutile questionOption_DC078BDA_A40F_B766_41E1_893074B7AC0B.text = rutile questionOption_63018B91_BB90_8B85_41DA_F578BF3566B2.text = sandstone questionOption_62A48AF0_BB91_9583_41E6_1160AD056DC6.text = sandstone questionOption_DDE43039_C3E9_53A9_41E1_A93406FD321B.text = sedimentary layers deposited, then folded and foliated, then intruded by a felsic dyke questionOption_DDE58038_C3E9_53B7_41D5_72F5E192EC8C.text = sedimentary layers deposited, then intruded by a felsic dyke, then folded, then foliated questionOption_0D931B97_AC06_B7EE_41C6_0C29D27AECF1.text = settling of crystals at the base of a magma chamber questionOption_0D931B97_AC06_B7EE_41C6_0C29D27AECF1.text = settling of crystals at the base of a magma chamber questionOption_AE6A3900_B890_9483_41A4_5AD55EADA4C8.text = shale questionOption_EA8D7540_A41B_38D0_41D7_B7DE31D81D87.text = sharp and curved questionOption_EA8EC53E_A41B_38B0_41B0_F149E78BF4AE.text = sharp and straight questionOption_9B5E53F4_A402_B722_41D8_DB0E7938B400.text = sharply truncated and offset questionOption_9B5E53F4_A402_B722_41D8_DB0E7938B400.text = sharply truncated and offset questionOption_BF1A3ED1_B990_8D85_41D0_FA815419BFB8.text = shear bands questionOption_ACC233B3_C56E_D4B9_41E6_3D348BC89087.text = single crystal of quartz questionOption_1C41E3B6_AC05_772E_41AC_9A835B3E0FA2.text = slightly enriched LREE and a negative Nb+Ta anomaly questionOption_1C41E3B6_AC05_772E_41AC_9A835B3E0FA2.text = slightly enriched LREE and a negative Nb+Ta anomaly questionOption_2E83EC25_C4F7_A8B4_41B0_CA3C9C112DF4.text = slow cooling causing polygonal cooling joints questionOption_03BFEC70_AC05_F122_41E1_E88435383F51.text = slow crystallization and intergrowth in a magma chamber questionOption_03BFEC70_AC05_F122_41E1_E88435383F51.text = slow crystallization and intergrowth in a magma chamber questionOption_EA847516_A41B_3870_41E0_A5C17D485D89.text = smoothly-curved and folded questionOption_C5406746_B991_BC8F_41E7_1CE82656741E.text = soft sediment deformation questionOption_BF1A3ED3_B990_8D85_41E5_D69495C3AD08.text = spaced axial planar cleavage questionOption_A451F59D_CD95_9B94_419A_F6DB26065FA7.text = spheroidal, nodular questionOption_617265F1_BB8F_9F85_41A8_7961D3BB9D19.text = spinifex questionOption_D860F601_A402_B0E2_41E4_1EBAF2FE38F8.text = spinifex basalt questionOption_D860F601_A402_B0E2_41E4_1EBAF2FE38F8.text = spinifex basalt questionOption_D3699092_A4FD_B1E6_41D3_3D5E34B71F4A.text = steeply dipping NNW questionOption_BEE50F87_B8B0_8B8D_41E6_B6E0836251DD.text = steeply dipping NNW questionOption_D3699092_A4FD_B1E6_41D3_3D5E34B71F4A.text = steeply dipping NNW questionOption_BEE50F88_B8B0_8B83_41E4_A16BA611C91A.text = steeply dipping W questionOption_D3E0EDE2_A402_9326_41D2_5E0ACDB19BAE.text = steeply plunging questionOption_D3E0EDE2_A402_9326_41D2_5E0ACDB19BAE.text = steeply plunging questionOption_DD3B920F_A406_90FE_41E0_D5FD93A6C865.text = steeply plunging questionOption_D3E0EDE2_A402_9326_41D2_5E0ACDB19BAE.text = steeply plunging questionOption_DD3B920F_A406_90FE_41E0_D5FD93A6C865.text = steeply plunging questionOption_D3E0EDE2_A402_9326_41D2_5E0ACDB19BAE.text = steeply plunging questionOption_05792037_AC06_912E_41E3_202EC71CF254.text = stepped questionOption_05792037_AC06_912E_41E3_202EC71CF254.text = stepped questionOption_EA8D6541_A41B_38D0_41B6_CA70657BC553.text = stepped questionOption_BF1A3ED5_B990_8D8D_41E7_05D46E697FE2.text = stretching lineation questionOption_02AD7126_AC05_B32E_41DB_6BDC3BB42B9D.text = strongly enriched in HREE and depleted LREE questionOption_02AD7126_AC05_B32E_41DB_6BDC3BB42B9D.text = strongly enriched in HREE and depleted LREE questionOption_E403049A_A403_91E6_41E2_A5D51D8684DC.text = strongly light-REE enriched questionOption_E403049A_A403_91E6_41E2_A5D51D8684DC.text = strongly light-REE enriched questionOption_1FC51999_AC02_B3E2_41C3_D692E5261811.text = strongly negative Ti and Nb+Ta anomalies questionOption_1FC51999_AC02_B3E2_41C3_D692E5261811.text = strongly negative Ti and Nb+Ta anomalies questionOption_0ABCA93E_A1C2_8CC0_41DD_00AE84BB3A58.text = sub-alkaline and transitional sub-alkaline to alkaline questionOption_D0922077_A4FD_F12E_41D9_A700F83576F9.text = sub-vertical questionOption_D0922077_A4FD_F12E_41D9_A700F83576F9.text = sub-vertical questionOption_A451759C_CD95_9B94_41CE_F0C4DE2B61F1.text = tabular, prismatic questionOption_DD40FC99_C3E9_7369_41E7_70298C074840.text = take samples from old workings and analyse them in the laboratory questionOption_C540B745_B991_BC8D_41BC_47B68C156D63.text = tectonic deformation questionOption_F7983B8A_A402_97E6_41D0_4372C6AECD16.text = the data points are reasonably consistent within analytical precision, and the age is acceptable. questionOption_F7983B8A_A402_97E6_41D0_4372C6AECD16.text = the data points are reasonably consistent within analytical precision, and the age is acceptable. questionOption_F7CE2A57_A402_916E_41D7_752ABE0FF332.text = the data points are tightly in agreement yielding a robust and precise mean age questionOption_F7CE2A57_A402_916E_41D7_752ABE0FF332.text = the data points are tightly in agreement yielding a robust and precise mean age questionOption_F65D0713_A402_90E6_41DC_D2346BC76CC1.text = the data points are wildly different and indicating the mean age is not acceptable questionOption_F65D0713_A402_90E6_41DC_D2346BC76CC1.text = the data points are wildly different and indicating the mean age is not acceptable questionOption_DFD772E6_A43D_B12E_41CF_854019E5CEC7.text = the folds formed by an axial slip mechanism questionOption_DFD772E6_A43D_B12E_41CF_854019E5CEC7.text = the folds formed by an axial slip mechanism questionOption_F58CD415_C369_3379_41E1_6AB6E94682E8.text = the rock is rich in magnesium questionOption_F5FA6418_C369_3377_41C9_5509987DCCB8.text = the rock was an intrusive igneous rock questionOption_F5FA4419_C369_3369_41E2_BBE8C9B0D201.text = the rock was cooled rapidly questionOption_F5FAE417_C369_3379_41C3_789091DA0567.text = the rock was originally deposited on the ocean floor questionOption_9E1825E6_A9B5_DA27_41C1_309D0E2CFDF8.text = they are felsic questionOption_9E0205E7_A9B5_DA25_41DC_03627F35D9EB.text = they are mafic questionOption_BEA1F341_B8B3_9485_41DB_4D2112B96FA2.text = they do not contain alkali-bearing minerals questionOption_BEA1F33F_B8B3_94FD_41E3_EDDD283187B0.text = they do not contain quartz questionOption_BEA1F342_B8B3_9487_41DF_8525EB289575.text = they have been contaminated by felsic crustal material questionOption_BEA1F344_B8B3_9483_41E5_838FA986B3E5.text = they have been crystallized from highly evolved magma questionOption_FCA37EC7_A402_F16E_41DF_3D74D2CD4E7C.text = thinly bedded questionOption_F897DC5F_A40E_B11E_412A_06490F5472FC.text = thinly bedded questionOption_FCA37EC7_A402_F16E_41DF_3D74D2CD4E7C.text = thinly bedded questionOption_F897DC5F_A40E_B11E_412A_06490F5472FC.text = thinly bedded questionOption_D24CE79C_A40D_9FE2_41E2_67D5A33C771D.text = tight questionOption_D24CE79C_A40D_9FE2_41E2_67D5A33C771D.text = tight questionOption_D24CE79C_A40D_9FE2_41E2_67D5A33C771D.text = tight questionOption_DF6E1D72_A406_9326_41D7_42F51EB54BAD.text = tight questionOption_D24CE79C_A40D_9FE2_41E2_67D5A33C771D.text = tight questionOption_D24CE79C_A40D_9FE2_41E2_67D5A33C771D.text = tight questionOption_DF6E1D72_A406_9326_41D7_42F51EB54BAD.text = tight questionOption_DF6E1D72_A406_9326_41D7_42F51EB54BAD.text = tight questionOption_D24CE79C_A40D_9FE2_41E2_67D5A33C771D.text = tight questionOption_D24CE79C_A40D_9FE2_41E2_67D5A33C771D.text = tight questionOption_D24CE79C_A40D_9FE2_41E2_67D5A33C771D.text = tight questionOption_DF6E1D72_A406_9326_41D7_42F51EB54BAD.text = tight questionOption_EAFE8514_A41B_3870_41D3_993CA5E02DB4.text = truncational and faulted questionOption_0ABC7941_A1C2_8F40_41D2_1AFD96638754.text = ultra-alkaline questionOption_D3A4D7E4_A402_FF22_41E3_24BD0DCECE64.text = ultramafic questionOption_DDA80240_A406_B162_41D2_621B7996C51E.text = ultramafic questionOption_A2825360_CD94_F8AC_41D4_9728FE3B9FD6.text = ultramafic questionOption_DDA80240_A406_B162_41D2_621B7996C51E.text = ultramafic questionOption_94A568D1_A994_EA7D_41E3_39FDDD8D6637.text = ultramafic questionOption_DDA80240_A406_B162_41D2_621B7996C51E.text = ultramafic questionOption_DDA80240_A406_B162_41D2_621B7996C51E.text = ultramafic questionOption_D3A4D7E4_A402_FF22_41E3_24BD0DCECE64.text = ultramafic questionOption_DDA80240_A406_B162_41D2_621B7996C51E.text = ultramafic questionOption_D3A4D7E4_A402_FF22_41E3_24BD0DCECE64.text = ultramafic questionOption_D3A4D7E4_A402_FF22_41E3_24BD0DCECE64.text = ultramafic questionOption_DDA80240_A406_B162_41D2_621B7996C51E.text = ultramafic questionOption_DDA80240_A406_B162_41D2_621B7996C51E.text = ultramafic questionOption_DDA80240_A406_B162_41D2_621B7996C51E.text = ultramafic questionOption_AD64B82D_C56E_F3A9_41E3_1FA2EA03FAE7.text = ultramafics questionOption_D30BB42D_A403_B122_41DE_DF91EA5C589E.text = vertical questionOption_D30BB42D_A403_B122_41DE_DF91EA5C589E.text = vertical questionOption_D30BB42D_A403_B122_41DE_DF91EA5C589E.text = vertical questionOption_DD6E2F3C_A407_6F22_41D8_A7B764481369.text = vertical questionOption_BEE50F85_B8B0_8B8D_41E2_95DCFB77CE8A.text = vertical questionOption_DD6E2F3C_A407_6F22_41D8_A7B764481369.text = vertical questionOption_D30BB42D_A403_B122_41DE_DF91EA5C589E.text = vertical questionOption_DD45E654_A40F_9162_41E0_65BFC2C80327.text = vesicular questionOption_DC811534_A402_9322_41C9_E7B4CB438F04.text = vesicular questionOption_DC811534_A402_9322_41C9_E7B4CB438F04.text = vesicular questionOption_DD45E654_A40F_9162_41E0_65BFC2C80327.text = vesicular questionOption_DD45E654_A40F_9162_41E0_65BFC2C80327.text = vesicular questionOption_DC811534_A402_9322_41C9_E7B4CB438F04.text = vesicular questionOption_DD45E654_A40F_9162_41E0_65BFC2C80327.text = vesicular questionOption_DC811534_A402_9322_41C9_E7B4CB438F04.text = vesicular questionOption_DB93AAEB_A402_9126_41DA_9CD413D64814.text = vesicular basalt questionOption_DB93AAEB_A402_9126_41DA_9CD413D64814.text = vesicular basalt questionOption_2955CD80_C4F4_A86C_41C8_3D8FACF4B7FA.text = volcanic arc (slab melting) questionOption_48BA4AA6_BB91_958F_41AC_F4B6FEC2E981.text = was extruded as lava as lava that was supercooled from high temperatures questionOption_517991EC_BB90_B783_41E2_A999F3FF33B9.text = was extruded as lava that cooled rapidly questionOption_4E7978EE_BB93_959F_41D3_18E674442371.text = was extruded as lava that cooled rapidly questionOption_49668C55_BB90_8C8D_41BF_D11F7E8B2B1D.text = was extruded as lava that cooled rapidly questionOption_4B388A4E_BB91_B49F_41E4_A3779FD12E04.text = was extruded as lava that cooled rapidly questionOption_48BBDAA7_BB91_958D_41D3_E41AD3D4EFB4.text = was extruded as lava that cooled rapidly questionOption_4A97C997_BB91_978D_41CD_74456A28AD8D.text = was extruded as lava that cooled rapidly questionOption_4A4DF4DB_BB90_7D85_41C5_74743FD53DA0.text = was extruded as lava that cooled rapidly questionOption_49664C53_BB90_8C85_41E6_90473F2119F6.text = was extruded as lava that was supercooled from high temperatures questionOption_5179A1EA_BB90_B787_41E0_7A5B1BCA495C.text = was extruded as lava that was supercooled from high temperatures questionOption_49640C59_BB90_8C85_41D2_35617D18BC46.text = was extruded in a subaqueous environment questionOption_4E78B8F0_BB93_9583_41C3_FEE2C4DBC63B.text = was extruded in a subaqueous environment questionOption_517971EE_BB90_B79F_41D6_08582F9E689A.text = was extruded in a subaqueous environment questionOption_4A96199C_BB91_9783_41D4_8D0D8396FD27.text = was extruded in a subaqueous environment questionOption_4B39BA51_BB91_B485_41E5_F0C14C9F7105.text = was extruded in a subaqueous environment questionOption_48BA4AA9_BB91_9585_41A6_3EA41A4E4B70.text = was extruded in a subaqueous environment questionOption_4A4C24DE_BB90_7DBF_41C4_F90D44EEFBF6.text = was extruded in a subaqueous environment questionOption_9AB6CD0B_A41E_B0E6_41E1_932E938443F9.text = weakly light-REE enriched questionOption_9AB6CD0B_A41E_B0E6_41E1_932E938443F9.text = weakly light-REE enriched questionOption_D93F9453_A403_7166_41DB_6DF48A0376A7.text = yes questionOption_D93F9453_A403_7166_41DB_6DF48A0376A7.text = yes questionOption_2FCB0C00_C4F7_A86C_41D7_5D0D30D1C7DC.text = young towards the east questionOption_2FCA7BFF_C4F7_AF94_41E7_18F34F0F9173.text = young towards the north questionOption_2FCB0C01_C4F7_A86C_41C9_742666708EF9.text = young towards the south questionOption_2FCB2C02_C4F7_A86C_41E0_83292FF06250.text = young towards the west questionOption_A3BB5DB0_C56F_ECB7_419F_FDD75D645F00.text = younging to the east questionOption_A3BB6DB1_C56F_ECB9_41E0_3484096BE64B.text = younging to the north questionOption_A3841DB3_C56F_ECB9_41DA_12FBAD284F7E.text = younging to the south questionOption_A3BA6DAF_C56F_ECA9_41E5_CFA2C0E2394C.text = younging to the west questionOption_C0BEC2D4_A407_9162_41B3_880FA7E682B6.text = ‘m’ folds questionOption_C0BEC2D4_A407_9162_41B3_880FA7E682B6.text = ‘m’ folds questionOption_C0DB8266_A406_912E_41A5_321E3BE4C0C5.text = ‘s’ folds questionOption_C0DB8266_A406_912E_41A5_321E3BE4C0C5.text = ‘s’ folds questionOption_C7163798_A406_9FE2_41E3_EE7B139E70E6.text = ‘z’ folds questionOption_C7163798_A406_9FE2_41E3_EE7B139E70E6.text = ‘z’ folds ### Question question_C5473744_B991_BC83_41CA_B2F6055E2EB9.title = Q 1/1 - Layers have been pulled apart to form lozenge-shaped blocks. What process could do this? question_1D5BF762_8030_A270_4198_6E8E50F5C34B.title = Q 1/1 - The image shows a dark red-weathering rock fragment inclusion – a xenolith. \ Based on its weathering colour, what was likely to be its original composition? question_49665C53_BB90_8C85_41C1_574719CD05AE.title = Q 1/1 - What inferences can you make from the presence of spinifex texture? question_A5E045EF_CD94_7BB4_41C9_5490ECBA0820.title = Q 1/1 - What interpretations can be made from field relationships among rock types shown on the map of location 7? question_29554D7D_C4F4_A894_41C7_1DE071658053.title = Q 1/1 - From the trace element geochemistry data of Smithies et al. (2018), what were likely magmatic source(s) of rocks from the Kalgoorlie-Kambalda greenstone belt? question_2CE4CD5B_C4F4_689C_41E1_EBD2B6D0E5AF.title = Q 1/1 - Approximately how large are the pillows in this location? question_2FCA4BFF_C4F7_AF94_41D8_3D138CA06827.title = Q 1/1 - Pillows have domed tops and pinched bases (keels). Using the compass and the shape of the pillows, decipher the younging direction. question_0F692FC7_BB90_8B8D_41CE_5FBB4AC0E34A.title = Q 1/1 - This coarse grained, crystalline rock predominantly contains large (up to 2 cm long) lath-shaped milky-white crystals with visible twins. Identify the mineral. question_4B3B3A4D_BB91_B49D_41C3_D4CF91F480BB.title = Q 1/1 - This rock is <1 m wide and cross cuts the speckled rock type. What inference can you make about the formation of this rock type from its texture, composition, and field relationship? question_62A95AED_BB91_959D_41CA_E49196EC74E8.title = Q 1/1 - This rock is fine grained, grey green on a fresh surface, massive, crystalline, and aphyric. Identify this rock type. question_63017B8E_BB90_8B9F_41D0_8272D5580D8E.title = Q 1/1 - This rock is medium grained, massive, crystalline, and ~50% plagioclase and ~50% mafic minerals. Identify this rock type. question_88312B0E_C329_356B_41C8_CA06F0FC53A5.title = Q 1/1 - Using the compass, estimate the approximate trend of the foliation. question_E79189DD_B9F0_F7BD_41DF_75F2D42AC089.title = Q 1/1 - Using the compass, what is the approximate trend of the antiform? question_EAFE6284_A41B_5850_41D7_AA4CA9B2EDC3.title = Q 1/1 - Using the concept of Anderson’s theory of dykes and sills and the orientation of the dyke, infer the orientation of the minimum principal stress (sigma 3) during dyke emplacement. question_1BB82470_9EC6_8540_41C7_FFFA1D2DE68C.title = Q 1/1 - Using the concept of Anderson’s theory of faulting, your mapped orientation of faults, and assuming displacement is predominantly strike-slip, infer the orientation of the principal stresses (sigmas 1, 2 and 3) during faulting. question_F58D1415_C369_3379_41E6_0502ED8B3461.title = Q 1/1 - What can you infer from the presence of talc at this outcrop? question_4A965996_BB91_978F_41E4_C6091B66AAD6.title = Q 1/1 - What inference can be made about the formation of this rock type from its texture? question_4A4C74D9_BB90_7D85_41E0_6FC305CB6CAB.title = Q 1/1 - What inference can be made about the formation of this rock type? question_5179D1EA_BB90_B787_41DC_758483DFF1E8.title = Q 1/1 - What inference can be made about the formation of this rock? question_48BA5AA6_BB91_958F_416E_621F1F0A5288.title = Q 1/1 - What inference can be made about the formation of this rock? question_4E7998ED_BB93_959D_41B2_CD22559E47C0.title = Q 1/1 - What inference can be made about the formation of this rock? \ \ question_DDE46038_C3E9_53B7_41DB_52C94F27A4AB.title = Q 1/1 - What inferences can be made about the relative geological history from this outcrop? question_E47F8C49_B9F1_8C85_41D0_246D8B95347F.title = Q 1/1 - What is the correct younging symbol assuming fining-upwards of the graded bedding? question_BEE50F83_B8B0_8B85_41E2_184DEE5440C5.title = Q 1/1 - Which best describes the orientation of bedding in these metasedimentary rocks? question_EAFEC514_A41B_3870_41C3_8B9BE1D62094.title = Q 1/1 - Which describes and explains the nature of the offset of the dyke in this locality? question_A5184260_CD94_98AC_41D8_762F12061F78.title = Q 1/1 - Which interpretations are consistent with your findings from the three rock types at this locality? question_A3BBFDAF_C56F_ECA9_41D8_B3C1F3A5A71E.title = Q 1/1 -The shapes of the pillows define domes (convex pillow tops) and keels (pinched pillow bases). Using your interpretive sketch, interpret the way up from the pillow forms. question_A2BC80DC_CD94_9994_41D8_D7D5281C7D66.title = Q 1/1 – This igneous rock type comprises an entirely blocky green crystal of pyroxene. Which term best classifies this rock type? question_60A8D8B6_BB8F_958F_41DD_32CDD00A9084.title = Q 1/2 - Using the compass, what is the approximate trend of the contact between the rock types? question_EB894F10_AAAC_E7FB_41D3_7D4DE5A6E342.title = Q 1/2 - What is the strike of bedding? question_A451259B_CD95_9B9C_41D1_2507F1E17507.title = Q 1/2 - What terms best describe the form of pale green minerals? question_9ECCB034_B970_F483_41E2_E55B622FDDB9.title = Q 1/2 - To the left of the compass is a small channel bedform. What does this imply about the environment of deposition? question_BF1A3ED1_B990_8D85_41CA_2B3486E8C69C.title = Q 1/2 - A foliation can be seen in the hinge zone of this fold layered metasedimentary rock. What best describes this foliation? question_A2FC1D02_CD94_A86C_41C4_281A99723208.title = Q 1/2 - Give a field name for this igneous rock which is fine grained, aphyric, green-grey, and weathers into smooth rounded boulders. question_A424D6DA_CD95_F99C_41E8_6EF2C4ADB92F.title = Q 1/2 - How does the silica and total alkali composition of pegmatitic gabbro sample MH58 compare to other mafic rocks in the area? question_DD470C97_C3E9_7379_41E0_4DBDA70ECB8A.title = Q 1/2 - How would you best go about deciphering the geological reasons why old timers found gold where they did. question_AE6B58FD_B890_957D_41C5_9D37129A7FF8.title = Q 1/2 - Identify the elongate clasts in this image. question_C1C0E823_AA93_E9DD_41E0_486D968DAB27.title = Q 1/2 - Identify the structure that is responsible for truncating layers in this location? question_BEE2D25F_B8B1_94BD_41D8_47AF8A09BA83.title = Q 1/2 - This felsic dyke has extruded metasedimentary rocks. Using the compass what is the approximate orientation of the foliations in the lower left of the image? question_6172D5EF_BB8F_9F9D_41CF_820B65CDEF7A.title = Q 1/2 - This green, fine-grained crystalline rock contains abundant large (up to 5cm long), needle-shaped (acicular) crystals arranged distinctively in a random and interlocking way. Which term best describes this texture? question_AC58A1F1_C56F_54B9_41E3_5EBEA7CE6ED9.title = Q 1/2 - Varioles are pale green spherulitic, dumb-bell, and globular forms. Estimate the proportion of this rock comprised of varioles. question_2E829C22_C4F7_A8AC_41E6_FF4717B0009C.title = Q 1/2 - What environment can be interpreted from the presence of pillow structures? question_166F7344_8031_E3B0_41DF_04F82E2C3785.title = Q 1/2 - What is the apparent offset of the dyke in this locality? question_E34EB91A_B9F0_B487_41D5_E4432EAFB653.title = Q 1/2 - What is the approximate trend of the axial trace of the small scale folds? question_1FCC1ABE_8030_E2D0_41D5_998C2A704CF0.title = Q 1/2 - What is the form of the small black crystals seen in the image? question_C0BF8511_AB6D_FBFD_41E4_C88DE037ADDD.title = Q 1/2 - What structures are present in the layer between the white arrows? question_EA80153C_A41B_38B0_41CE_58F71FB01416.title = Q 1/2 - Which best describes the nature of contact? question_BF090353_B970_7485_4199_497441799472.title = Q 1/2 - Which best describes the texture of the rock type on the right? question_A3CC9EBF_C56F_2CA9_41DD_81B9BB018BFB.title = Q 1/2 - Which is the best description of the rinds of the pillows? question_BEA1F33F_B8B3_94FD_41E0_15DE20766BD6.title = Q 1/2 - Why do pyroxenites plot along the x-axis? question_AD64C82C_C56E_F3AF_41D9_1F0911D2A670.title = Q 1/2 - With which group of rocks does a variolitic sample from this locality (MH30) have the closest affinity on the trace element diagram. question_D45C3711_B990_7C85_41E5_4E75A4ADC112.title = Q 1/3 - Approximately how thick is the in situ quartz vein? question_94ABF8CD_A994_EA65_41E1_642C8A2E2D18.title = Q 1/3 - Classify the pale pebble clasts in this domain. question_BE9FC441_B88F_FC85_41D9_2B7210A45E76.title = Q 1/3 - Sequence the samples from the least evolved to the most evolved. question_BF1A5689_B990_9D85_41DA_6D8459BA5D7A.title = Q 1/3 - Several fold hinges are preserved at this outcrop. What is the approximate trend of the axial surfaces? question_A282B35D_CD94_F894_41CD_69B0A4E30CCC.title = Q 1/3 - This igneous rock type contains ~50% plagioclase and ~50% pyroxene. How is it classified? question_9E1865E6_A9B5_DA27_41DF_AFB7D167378E.title = Q 1/3 - What do the pale colours of the rock layers imply? question_DD37AE1F_C3E9_2F69_41E2_1DCC0BB073C4.title = Q 1/3 - Which term best describes the geometry of the small folds localized in the layers above the compass? question_A5992150_CD95_B8EC_41CB_048B0FE9FC53.title = Q 1/3 - Which term describes the texture defined by the shapes of pseudomorphed primary pyroxene grains in this location? question_0C8A0BA5_A1C2_83C0_41C9_97DCE5A416B2.title = Q 1/4 - Study the Tera-Wasserburg diagram of zircon U-Pb data from felsic dyke sample MH35. Many data points are discordant. What reason can cause data to be spread in the direction of arrows, A, B and C. question_ACC223B2_C56E_D4BB_41DB_0455BFC38384.title = Q 1/4 - From the optical photomicrograph of the variolitic basalt, how would you describe the texture of the varioles? question_0ABCB93E_A1C2_8CC0_41DA_6E2C9B62B3C8.title = Q 1/4 - This TAS diagram shows whole-rock geochemistry of several other porphyritic felsic dykes exposed within 300 m of this locality. In terms of igneous series, how are these rocks classified? question_58B4FD27_BBB1_8C8D_41C6_F6E501D879D4.title = Q 1/4 - This rock type contains <5% milky-white weathering prismatic crystals up to 3mm long. question_BF1A1E4A_B990_8C87_41DD_36EA26667863.title = Q 1/4 - Using the compass, what is the approximate trend of the axial surface of this fold? question_21F9F5F4_B88F_9F83_41DE_971D28103FF8.title = Q 1/5 - This rock type is green on a fresh surface and predominantly comprises medium grained stubby prismatic green crystals. Identify this mineral. question_FB057758_EC02_C9F7_41E8_C6D0A92196E2.title = Q 1/6 - The larger red-wearing crystals (phenocrysts) in this rock are prismatic and have two cleavages almost at 90 degrees. Which mineral are these most likely to be? question_768B6B74_AC02_9722_41C0_20F93B311A9C.title = Q 2/2 - Use the compass to measure the trend of this structure. question_768B6B74_AC02_9722_41C0_20F93B311A9C.title = Q 2/2 - Use the compass to measure the trend of this structure. question_DFB7188B_A402_91E6_41E2_06FFF1F0C2E4.title = Q 2/2 - Does the felsic dyke cross cut the foliation? question_DFB7188B_A402_91E6_41E2_06FFF1F0C2E4.title = Q 2/2 - Does the felsic dyke cross cut the foliation? question_DD78089E_A407_B11E_41D3_AA8B7A431569.title = Q 2/2 - Given that the boundary can be constrained to within 10 cm here, what type of boundary symbol should be shown when mapping at a 1:2000 scale? question_DD78089E_A407_B11E_41D3_AA8B7A431569.title = Q 2/2 - Given that the boundary can be constrained to within 10 cm here, what type of boundary symbol should be shown when mapping at a 1:2000 scale? question_9B72F05B_A403_7166_41E0_1C8559C5BD17.title = Q 2/2 - How would you describe the nature of the offset dyke segments? question_9B72F05B_A403_7166_41E0_1C8559C5BD17.title = Q 2/2 - How would you describe the nature of the offset dyke segments? question_DF183499_A40D_B1E5_41DC_C7C71D98B19F.title = Q 2/2 - How would you prioritise geological field mapping tasks to explore for more orogenic gold deposits? question_DF183499_A40D_B1E5_41DC_C7C71D98B19F.title = Q 2/2 - How would you prioritise geological field mapping tasks to explore for more orogenic gold deposits? question_06E5845C_AC05_7162_41BF_E92D166E0B75.title = Q 2/2 - Identify the bladed crystals with simple twins and third order interference colours. question_06E5845C_AC05_7162_41BF_E92D166E0B75.title = Q 2/2 - Identify the bladed crystals with simple twins and third order interference colours. question_701F20EE_AC7E_F13E_41E3_500EED9712D2.title = Q 2/2 - Sequence the samples from the least evolved to the most evolved. question_701F20EE_AC7E_F13E_41E3_500EED9712D2.title = Q 2/2 - Sequence the samples from the least evolved to the most evolved. question_29C6F7E4_A405_9F22_41E0_0FBAA1B22416.title = Q 2/2 - The variolitic sample MH30 is enriched in silica relative to other basaltic rocks in the area. What could be reason for this? question_29C6F7E4_A405_9F22_41E0_0FBAA1B22416.title = Q 2/2 - The variolitic sample MH30 is enriched in silica relative to other basaltic rocks in the area. What could be reason for this? question_4BA9BDAD_BA1A_8314_41E1_2D1D157949C0.title = Q 2/2 - These crystals have been oxidised in the weathered zone. What mineral could these have been? question_4BA9BDAD_BA1A_8314_41E1_2D1D157949C0.title = Q 2/2 - These crystals have been oxidised in the weathered zone. What mineral could these have been? question_D94F5677_A406_912E_41DD_A14CAD167E03.title = Q 2/2 - Using the compass, what is the approximate trend of this foliation? question_D94F5677_A406_912E_41DD_A14CAD167E03.title = Q 2/2 - Using the compass, what is the approximate trend of this foliation? question_2A3EB896_A406_B1EE_41D8_32DBDDDFD0A9.title = Q 2/2 - Varioles are paler than the surrounding rock. What can be inferred from this? question_2A3EB896_A406_B1EE_41D8_32DBDDDFD0A9.title = Q 2/2 - Varioles are paler than the surrounding rock. What can be inferred from this? question_E84857E0_A406_BF22_41C5_1CBB0489E6DA.title = Q 2/2 - What is the approximate trend of the contract? question_E84857E0_A406_BF22_41C5_1CBB0489E6DA.title = Q 2/2 - What is the approximate trend of the contract? question_CEB14DA2_A405_9326_41DA_DADBBB4DB690.title = Q 2/2 - What is the asymmetry of the small scale folds? question_CEB14DA2_A405_9326_41DA_DADBBB4DB690.title = Q 2/2 - What is the asymmetry of the small scale folds? question_F8EF58CD_A402_9162_41D4_90834D4D27B1.title = Q 2/2 - What is the dip and dip direction of bedding? question_F8EF58CD_A402_9162_41D4_90834D4D27B1.title = Q 2/2 - What is the dip and dip direction of bedding? question_356636B2_A403_9126_41C3_B5B285D44860.title = Q 2/2 - What is the most likely cause of the laminations at pillow margins? question_356636B2_A403_9126_41C3_B5B285D44860.title = Q 2/2 - What is the most likely cause of the laminations at pillow margins? question_F9C17A9A_A43F_71E6_41DF_A83E89FFF2DD.title = Q 2/2 - What process could have made the clasts be elongate like this? question_F9C17A9A_A43F_71E6_41DF_A83E89FFF2DD.title = Q 2/2 - What process could have made the clasts be elongate like this? question_1017FBC9_AC02_B762_41CC_1405591CF913.title = Q 2/2 - What tectonic environment would be compatible with the presence of pillow lava? question_1017FBC9_AC02_B762_41CC_1405591CF913.title = Q 2/2 - What tectonic environment would be compatible with the presence of pillow lava? question_03C33AC8_AC02_9162_41C6_3F1158A48446.title = Q 2/2 - What term describes curved fracture surfaces preserved by this rock type? question_03C33AC8_AC02_9162_41C6_3F1158A48446.title = Q 2/2 - What term describes curved fracture surfaces preserved by this rock type? question_D9E9231F_A402_971E_41A9_AA4C74E13609.title = Q 2/2 - Which best describes the orientation of the foliation in this ferruginised basalt? question_D9E9231F_A402_971E_41A9_AA4C74E13609.title = Q 2/2 - Which best describes the orientation of the foliation in this ferruginised basalt? question_1BDA4A29_AC03_9122_416A_50B32C51D5B0.title = Q 2/2 - Which description best fits the trace element distribution relative to MORB for pegmatitic gabbro sample HM58? question_1BDA4A29_AC03_9122_416A_50B32C51D5B0.title = Q 2/2 - Which description best fits the trace element distribution relative to MORB for pegmatitic gabbro sample HM58? question_DF4DC42E_A40E_913E_41CD_FB6B69CD6C69.title = Q 2/2 - Which field name best for this rock? question_DF4DC42E_A40E_913E_41CD_FB6B69CD6C69.title = Q 2/2 - Which field name best for this rock? question_C44B39A8_A40D_7322_41C2_A17FD07BD9CE.title = Q 2/2 - Which younging symbol is correct to indicate way-up from the channel bedform? question_C44B39A8_A40D_7322_41C2_A17FD07BD9CE.title = Q 2/2 - Which younging symbol is correct to indicate way-up from the channel bedform? question_FD45ECA4_A40D_7122_41C1_CB327D2B53EB.title = Q 2/2 - Which younging symbol is correct? question_FD45ECA4_A40D_7122_41C1_CB327D2B53EB.title = Q 2/2 - Which younging symbol is correct? question_FFE59A45_A40F_9162_41CB_E88A317515F3.title = Q 2/3 - What best describes the sedimentary structures? question_FFE59A45_A40F_9162_41CB_E88A317515F3.title = Q 2/3 - What best describes the sedimentary structures? question_DF6E9355_A406_B762_41E3_86C56F03C2A5.title = Q 2/3 - How is MH55 distinguishable from MH56 based on trace elements? question_DF6E9355_A406_B762_41E3_86C56F03C2A5.title = Q 2/3 - How is MH55 distinguishable from MH56 based on trace elements? question_FAE8F0D3_A406_9166_41DA_A8F00707FF96.title = Q 2/3 - Identify the mineral clast under the hand lens. question_FAE8F0D3_A406_9166_41DA_A8F00707FF96.title = Q 2/3 - Identify the mineral clast under the hand lens. question_057CE0CB_AC05_9165_41D9_2E4CB01EB925.title = Q 2/3 - This igneous rock contains crystals up to 10 cm long in a groundmass of ~0.5cm crystals. What term best classifies this texture? question_057CE0CB_AC05_9165_41D9_2E4CB01EB925.title = Q 2/3 - This igneous rock contains crystals up to 10 cm long in a groundmass of ~0.5cm crystals. What term best classifies this texture? question_C2DD92D7_A40D_916E_41CD_87388296F561.title = Q 2/3 - Use the compass to measure the strike of this quartz vein. question_DE25532E_A405_773E_41CC_2F8E35DAC26C.title = Q 2/3 - Using the compass, what is the approximate trend of the axial surface of these small folds? question_DEFA118B_A41E_93E6_41DD_E2449B3736BA.title = Q 2/3 - What is the approximate interlimb angle of the fold adjacent the compass? question_DEFA118B_A41E_93E6_41DD_E2449B3736BA.title = Q 2/3 - What is the approximate interlimb angle of the fold adjacent the compass? question_1F63120B_AC07_90E6_41C2_5C726D7DCC78.title = Q 2/3 - What process of formation can be inferred from this texture? question_1F63120B_AC07_90E6_41C2_5C726D7DCC78.title = Q 2/3 - What process of formation can be inferred from this texture? question_2B2B0259_A47F_F162_41E2_C1AB2C75E9E8.title = Q 2/4 - At this scale, describe the margins of the varioles. question_2B2B0259_A47F_F162_41E2_C1AB2C75E9E8.title = Q 2/4 - At this scale, describe the margins of the varioles. question_D2F522DD_A405_B162_41D5_27FB8C2B4584.title = Q 2/4 - Given that the surface with the compass is horizontal, and the fold hinge is exposed in the foreground, classify this fold based on the plunge of its hinge. question_D2F522DD_A405_B162_41D5_27FB8C2B4584.title = Q 2/4 - Given that the surface with the compass is horizontal, and the fold hinge is exposed in the foreground, classify this fold based on the plunge of its hinge. question_9AC71004_A41E_F0E2_41CD_DD88BFC1DB61.title = Q 2/4 - Which best describes the chondrite-normalised rare earth elements (REE) patterns preserved by these rocks? question_9AC71004_A41E_F0E2_41CD_DD88BFC1DB61.title = Q 2/4 - Which best describes the chondrite-normalised rare earth elements (REE) patterns preserved by these rocks? question_EB17C309_A40F_90E2_41CE_867EF32F5D58.title = Q 2/4 -The Tera-Wassenburg diagram shows the most concordant zircon U-Pb data from felsic dyke sample MH35. Which isotype system would be most suitable for calculating an age for this rock? question_EB17C309_A40F_90E2_41CE_867EF32F5D58.title = Q 2/4 -The Tera-Wassenburg diagram shows the most concordant zircon U-Pb data from felsic dyke sample MH35. Which isotype system would be most suitable for calculating an age for this rock? question_D0E2AC4E_A405_917E_41D5_1C9E8FA20AF0.title = Q 2/4 – What can be inferred from the pale colour of the groundmass of this fine grained, massive, crystalline rock type? question_D0E2AC4E_A405_917E_41D5_1C9E8FA20AF0.title = Q 2/4 – What can be inferred from the pale colour of the groundmass of this fine grained, massive, crystalline rock type? question_D89C453A_A402_9326_4196_5ACED10DED1C.title = Q 2/5 -This rock contains ~5% larger prismatic pale green crystals up to 1 cm long with two visible cleavages at ~90 degrees. Identify this mineral. question_D89C453A_A402_9326_4196_5ACED10DED1C.title = Q 2/5 -This rock contains ~5% larger prismatic pale green crystals up to 1 cm long with two visible cleavages at ~90 degrees. Identify this mineral. question_D8E350B9_A402_F122_41A6_B7D144FF2EDE.title = Q 2/6 - The smaller, dark green crystals in this rock form stubby prisms. Which mineral are these most likely to be? question_048DD54E_AC03_737E_41E1_5991C6822F19.title = Q 3/3 - What mineral has replaced (pseudomorphed) primary clinopyroxene grains? question_048DD54E_AC03_737E_41E1_5991C6822F19.title = Q 3/3 - What mineral has replaced (pseudomorphed) primary clinopyroxene grains? question_048DD54E_AC03_737E_41E1_5991C6822F19.title = Q 3/3 - What mineral has replaced (pseudomorphed) primary clinopyroxene grains? question_048DD54E_AC03_737E_41E1_5991C6822F19.title = Q 3/3 - What mineral has replaced (pseudomorphed) primary clinopyroxene grains? question_DCECB5AA_A402_B326_41D7_168C825276EF.title = Q 3/3 - Classify the fold adjacent the compass based on its interlimb angle. question_DCECB5AA_A402_B326_41D7_168C825276EF.title = Q 3/3 - Classify the fold adjacent the compass based on its interlimb angle. question_DCECB5AA_A402_B326_41D7_168C825276EF.title = Q 3/3 - Classify the fold adjacent the compass based on its interlimb angle. question_DCECB5AA_A402_B326_41D7_168C825276EF.title = Q 3/3 - Classify the fold adjacent the compass based on its interlimb angle. question_D224D2EE_A402_F13E_41D1_9C827C6A76DF.title = Q 3/3 - Depletion of heavy rare earth elements (HREE) is attributed to melt extraction from a source containing what mineral? question_D224D2EE_A402_F13E_41D1_9C827C6A76DF.title = Q 3/3 - Depletion of heavy rare earth elements (HREE) is attributed to melt extraction from a source containing what mineral? question_D224D2EE_A402_F13E_41D1_9C827C6A76DF.title = Q 3/3 - Depletion of heavy rare earth elements (HREE) is attributed to melt extraction from a source containing what mineral? question_D224D2EE_A402_F13E_41D1_9C827C6A76DF.title = Q 3/3 - Depletion of heavy rare earth elements (HREE) is attributed to melt extraction from a source containing what mineral? question_70080962_AC03_7326_41E2_D847A63436F1.title = Q 3/3 - The translucent grey mineral clast has a hexagonal shape and is resistant to weathering. Identify the mineral. question_70080962_AC03_7326_41E2_D847A63436F1.title = Q 3/3 - The translucent grey mineral clast has a hexagonal shape and is resistant to weathering. Identify the mineral. question_70080962_AC03_7326_41E2_D847A63436F1.title = Q 3/3 - The translucent grey mineral clast has a hexagonal shape and is resistant to weathering. Identify the mineral. question_70080962_AC03_7326_41E2_D847A63436F1.title = Q 3/3 - The translucent grey mineral clast has a hexagonal shape and is resistant to weathering. Identify the mineral. question_CFDDD82D_A402_9122_41DA_E690183F0378.title = Q 3/3 - Use the compass to measure the dip of this quartz vein. question_CFDDD82D_A402_9122_41DA_E690183F0378.title = Q 3/3 - Use the compass to measure the dip of this quartz vein. question_FA71D12E_A402_B33E_41E4_4966838333DF.title = Q 3/3 - What best describes the sedimentary structures? question_FA71D12E_A402_B33E_41E4_4966838333DF.title = Q 3/3 - What best describes the sedimentary structures? question_DCBBC707_A402_B0EE_41CD_D6065EEA893A.title = Q 3/3 - What inference can you make about the deformation that caused this style of folding? question_DCBBC707_A402_B0EE_41CD_D6065EEA893A.title = Q 3/3 - What inference can you make about the deformation that caused this style of folding? question_01158F15_AC0E_90E2_41E3_C8738FEFACD1.title = Q 3/3 - Which is the most suitable field name for this rock type? question_01158F15_AC0E_90E2_41E3_C8738FEFACD1.title = Q 3/3 - Which is the most suitable field name for this rock type? question_01158F15_AC0E_90E2_41E3_C8738FEFACD1.title = Q 3/3 - Which is the most suitable field name for this rock type? question_01158F15_AC0E_90E2_41E3_C8738FEFACD1.title = Q 3/3 - Which is the most suitable field name for this rock type? question_D8EC9498_A405_B1E2_41BB_F657F96D4B9A.title = Q 3/4 - Given that the surface with the compass is horizontal, and the fold hinge is exposed in the foreground, classify this fold based on the plunge of its hinge. question_D8EC9498_A405_B1E2_41BB_F657F96D4B9A.title = Q 3/4 - Given that the surface with the compass is horizontal, and the fold hinge is exposed in the foreground, classify this fold based on the plunge of its hinge. question_D8EC9498_A405_B1E2_41BB_F657F96D4B9A.title = Q 3/4 - Given that the surface with the compass is horizontal, and the fold hinge is exposed in the foreground, classify this fold based on the plunge of its hinge. question_D8EC9498_A405_B1E2_41BB_F657F96D4B9A.title = Q 3/4 - Given that the surface with the compass is horizontal, and the fold hinge is exposed in the foreground, classify this fold based on the plunge of its hinge. question_F6170770_A40D_BF22_41E3_60788D849E4C.title = Q 3/4 - The weighted mean zircon Pb-Pb age from felsic dyke sample MH35 has been calculated from the 7 most concordant data points as 2673 +/- 8 Ma. What do the MSWD and P values tell you about the statistical validity of this age? question_F6170770_A40D_BF22_41E3_60788D849E4C.title = Q 3/4 - The weighted mean zircon Pb-Pb age from felsic dyke sample MH35 has been calculated from the 7 most concordant data points as 2673 +/- 8 Ma. What do the MSWD and P values tell you about the statistical validity of this age? question_D2BB5E0D_A403_70E2_41DE_F45B70625327.title = Q 3/4 - What textural term is used to describe a rock with larger crystals in a crystalline groundmass? question_D2BB5E0D_A403_70E2_41DE_F45B70625327.title = Q 3/4 - What textural term is used to describe a rock with larger crystals in a crystalline groundmass? question_D2BB5E0D_A403_70E2_41DE_F45B70625327.title = Q 3/4 - What textural term is used to describe a rock with larger crystals in a crystalline groundmass? question_D2BB5E0D_A403_70E2_41DE_F45B70625327.title = Q 3/4 - What textural term is used to describe a rock with larger crystals in a crystalline groundmass? question_29B1542F_A405_B13E_41D6_9DF3B43ABD2F.title = Q 3/4 - What texture is visible in the varioles in cross polarized light? question_29B1542F_A405_B13E_41D6_9DF3B43ABD2F.title = Q 3/4 - What texture is visible in the varioles in cross polarized light? question_29B1542F_A405_B13E_41D6_9DF3B43ABD2F.title = Q 3/4 - What texture is visible in the varioles in cross polarized light? question_29B1542F_A405_B13E_41D6_9DF3B43ABD2F.title = Q 3/4 - What texture is visible in the varioles in cross polarized light? question_E6D29B5F_A405_771E_41DE_258EA00A3223.title = Q 3/4 - Which process can lead to this kind of HREE pattern? question_E6D29B5F_A405_771E_41DE_258EA00A3223.title = Q 3/4 - Which process can lead to this kind of HREE pattern? question_E6D29B5F_A405_771E_41DE_258EA00A3223.title = Q 3/4 - Which process can lead to this kind of HREE pattern? question_E6D29B5F_A405_771E_41DE_258EA00A3223.title = Q 3/4 - Which process can lead to this kind of HREE pattern? question_D2360AB3_A40D_7126_41DE_EDCC72503C03.title = Q 3/5 - What textural term is used to describe a rock with larger crystals in a crystalline groundmass? question_D2360AB3_A40D_7126_41DE_EDCC72503C03.title = Q 3/5 - What textural term is used to describe a rock with larger crystals in a crystalline groundmass? question_D2360AB3_A40D_7126_41DE_EDCC72503C03.title = Q 3/5 - What textural term is used to describe a rock with larger crystals in a crystalline groundmass? question_D2360AB3_A40D_7126_41DE_EDCC72503C03.title = Q 3/5 - What textural term is used to describe a rock with larger crystals in a crystalline groundmass? question_DFFF34D6_A402_B16E_41BC_FC0F832F8851.title = Q 3/6 - White-weathering plagioclase fills the gaps between the well-defined green and red-weathering crystals. What is the term for this? question_DFFF34D6_A402_B16E_41BC_FC0F832F8851.title = Q 3/6 - White-weathering plagioclase fills the gaps between the well-defined green and red-weathering crystals. What is the term for this? question_DBFB15B5_A40F_F322_41E2_425E47700A3A.title = Q 4/4 - Classify the fold based on its interlimb angle. question_DBFB15B5_A40F_F322_41E2_425E47700A3A.title = Q 4/4 - Classify the fold based on its interlimb angle. question_DBFB15B5_A40F_F322_41E2_425E47700A3A.title = Q 4/4 - Classify the fold based on its interlimb angle. question_DBFB15B5_A40F_F322_41E2_425E47700A3A.title = Q 4/4 - Classify the fold based on its interlimb angle. question_DBFB15B5_A40F_F322_41E2_425E47700A3A.title = Q 4/4 - Classify the fold based on its interlimb angle. question_DBFB15B5_A40F_F322_41E2_425E47700A3A.title = Q 4/4 - Classify the fold based on its interlimb angle. question_DBFB15B5_A40F_F322_41E2_425E47700A3A.title = Q 4/4 - Classify the fold based on its interlimb angle. question_DBFB15B5_A40F_F322_41E2_425E47700A3A.title = Q 4/4 - Classify the fold based on its interlimb angle. question_E919397F_A407_F31E_41D3_DA992EF2EF23.title = Q 4/4 - What inference can you make from this zircon Pb/Pb age? question_E919397F_A407_F31E_41D3_DA992EF2EF23.title = Q 4/4 - What inference can you make from this zircon Pb/Pb age? question_E919397F_A407_F31E_41D3_DA992EF2EF23.title = Q 4/4 - What inference can you make from this zircon Pb/Pb age? question_E919397F_A407_F31E_41D3_DA992EF2EF23.title = Q 4/4 - What inference can you make from this zircon Pb/Pb age? question_3435C0DA_A405_9166_41C4_25A08A60FC6D.title = Q 4/4 - What is the best interpretation of varioles and how they formed? question_3435C0DA_A405_9166_41C4_25A08A60FC6D.title = Q 4/4 - What is the best interpretation of varioles and how they formed? question_3435C0DA_A405_9166_41C4_25A08A60FC6D.title = Q 4/4 - What is the best interpretation of varioles and how they formed? question_3435C0DA_A405_9166_41C4_25A08A60FC6D.title = Q 4/4 - What is the best interpretation of varioles and how they formed? question_3435C0DA_A405_9166_41C4_25A08A60FC6D.title = Q 4/4 - What is the best interpretation of varioles and how they formed? question_3435C0DA_A405_9166_41C4_25A08A60FC6D.title = Q 4/4 - What is the best interpretation of varioles and how they formed? question_3435C0DA_A405_9166_41C4_25A08A60FC6D.title = Q 4/4 - What is the best interpretation of varioles and how they formed? question_3435C0DA_A405_9166_41C4_25A08A60FC6D.title = Q 4/4 - What is the best interpretation of varioles and how they formed? question_DB656644_A407_B162_41E2_955727B1EEAA.title = Q 4/4 - Which field term best fits this rock type? question_DB656644_A407_B162_41E2_955727B1EEAA.title = Q 4/4 - Which field term best fits this rock type? question_DB656644_A407_B162_41E2_955727B1EEAA.title = Q 4/4 - Which field term best fits this rock type? question_DB656644_A407_B162_41E2_955727B1EEAA.title = Q 4/4 - Which field term best fits this rock type? question_DB656644_A407_B162_41E2_955727B1EEAA.title = Q 4/4 - Which field term best fits this rock type? question_DB656644_A407_B162_41E2_955727B1EEAA.title = Q 4/4 - Which field term best fits this rock type? question_DB656644_A407_B162_41E2_955727B1EEAA.title = Q 4/4 - Which field term best fits this rock type? question_DB656644_A407_B162_41E2_955727B1EEAA.title = Q 4/4 - Which field term best fits this rock type? question_E073EFB1_A40E_AF22_41D6_95A61F40ED5A.title = Q 4/4 - Which process can lead to this kind of LREE pattern? question_E073EFB1_A40E_AF22_41D6_95A61F40ED5A.title = Q 4/4 - Which process can lead to this kind of LREE pattern? question_E073EFB1_A40E_AF22_41D6_95A61F40ED5A.title = Q 4/4 - Which process can lead to this kind of LREE pattern? question_E073EFB1_A40E_AF22_41D6_95A61F40ED5A.title = Q 4/4 - Which process can lead to this kind of LREE pattern? question_E073EFB1_A40E_AF22_41D6_95A61F40ED5A.title = Q 4/4 - Which process can lead to this kind of LREE pattern? question_E073EFB1_A40E_AF22_41D6_95A61F40ED5A.title = Q 4/4 - Which process can lead to this kind of LREE pattern? question_E073EFB1_A40E_AF22_41D6_95A61F40ED5A.title = Q 4/4 - Which process can lead to this kind of LREE pattern? question_E073EFB1_A40E_AF22_41D6_95A61F40ED5A.title = Q 4/4 - Which process can lead to this kind of LREE pattern? question_D395935F_A407_B71E_419E_D2F858131746.title = Q 4/5 - Classify this rock type. question_D395935F_A407_B71E_419E_D2F858131746.title = Q 4/5 - Classify this rock type. question_D395935F_A407_B71E_419E_D2F858131746.title = Q 4/5 - Classify this rock type. question_D395935F_A407_B71E_419E_D2F858131746.title = Q 4/5 - Classify this rock type. question_D395935F_A407_B71E_419E_D2F858131746.title = Q 4/5 - Classify this rock type. question_D395935F_A407_B71E_419E_D2F858131746.title = Q 4/5 - Classify this rock type. question_D395935F_A407_B71E_419E_D2F858131746.title = Q 4/5 - Classify this rock type. question_D395935F_A407_B71E_419E_D2F858131746.title = Q 4/5 - Classify this rock type. question_D0BB03C1_A40D_9762_41DA_29DA7FA1E92B.title = Q 4/6 - Classify this rock type. question_D0BB03C1_A40D_9762_41DA_29DA7FA1E92B.title = Q 4/6 - Classify this rock type. question_D0BB03C1_A40D_9762_41DA_29DA7FA1E92B.title = Q 4/6 - Classify this rock type. question_D0BB03C1_A40D_9762_41DA_29DA7FA1E92B.title = Q 4/6 - Classify this rock type. question_D6D4BBBE_A403_F71E_41B6_8FA1BF84BC11.title = Q 5/5 - Which name best classifies this rock type? question_D6D4BBBE_A403_F71E_41B6_8FA1BF84BC11.title = Q 5/5 - Which name best classifies this rock type? question_D6D4BBBE_A403_F71E_41B6_8FA1BF84BC11.title = Q 5/5 - Which name best classifies this rock type? question_D6D4BBBE_A403_F71E_41B6_8FA1BF84BC11.title = Q 5/5 - Which name best classifies this rock type? question_D6D4BBBE_A403_F71E_41B6_8FA1BF84BC11.title = Q 5/5 - Which name best classifies this rock type? question_D6D4BBBE_A403_F71E_41B6_8FA1BF84BC11.title = Q 5/5 - Which name best classifies this rock type? question_D6D4BBBE_A403_F71E_41B6_8FA1BF84BC11.title = Q 5/5 - Which name best classifies this rock type? question_D6D4BBBE_A403_F71E_41B6_8FA1BF84BC11.title = Q 5/5 - Which name best classifies this rock type? question_D6D4BBBE_A403_F71E_41B6_8FA1BF84BC11.title = Q 5/5 - Which name best classifies this rock type? question_D6D4BBBE_A403_F71E_41B6_8FA1BF84BC11.title = Q 5/5 - Which name best classifies this rock type? question_D6D4BBBE_A403_F71E_41B6_8FA1BF84BC11.title = Q 5/5 - Which name best classifies this rock type? question_D6D4BBBE_A403_F71E_41B6_8FA1BF84BC11.title = Q 5/5 - Which name best classifies this rock type? question_D6D4BBBE_A403_F71E_41B6_8FA1BF84BC11.title = Q 5/5 - Which name best classifies this rock type? question_D6D4BBBE_A403_F71E_41B6_8FA1BF84BC11.title = Q 5/5 - Which name best classifies this rock type? question_D6D4BBBE_A403_F71E_41B6_8FA1BF84BC11.title = Q 5/5 - Which name best classifies this rock type? question_D6D4BBBE_A403_F71E_41B6_8FA1BF84BC11.title = Q 5/5 - Which name best classifies this rock type? question_DC6C03F1_A402_9722_41CB_BE51A68C3733.title = Q 5/6 - Which describes the texture of this rock type? question_DC6C03F1_A402_9722_41CB_BE51A68C3733.title = Q 5/6 - Which describes the texture of this rock type? question_DC6C03F1_A402_9722_41CB_BE51A68C3733.title = Q 5/6 - Which describes the texture of this rock type? question_DC6C03F1_A402_9722_41CB_BE51A68C3733.title = Q 5/6 - Which describes the texture of this rock type? question_D8AC5D4D_A47E_F362_4196_1AFECC0762AD.title = Q 6/6 - Based on minerals present in the rock, which named best classifies this rock type. question_D8AC5D4D_A47E_F362_4196_1AFECC0762AD.title = Q 6/6 - Based on minerals present in the rock, which named best classifies this rock type. question_D8AC5D4D_A47E_F362_4196_1AFECC0762AD.title = Q 6/6 - Based on minerals present in the rock, which named best classifies this rock type. question_D8AC5D4D_A47E_F362_4196_1AFECC0762AD.title = Q 6/6 - Based on minerals present in the rock, which named best classifies this rock type. question_D8AC5D4D_A47E_F362_4196_1AFECC0762AD.title = Q 6/6 - Based on minerals present in the rock, which named best classifies this rock type. question_D8AC5D4D_A47E_F362_4196_1AFECC0762AD.title = Q 6/6 - Based on minerals present in the rock, which named best classifies this rock type. question_D8AC5D4D_A47E_F362_4196_1AFECC0762AD.title = Q 6/6 - Based on minerals present in the rock, which named best classifies this rock type. question_D8AC5D4D_A47E_F362_4196_1AFECC0762AD.title = Q 6/6 - Based on minerals present in the rock, which named best classifies this rock type. ### Question Screen quizQuestion_6BF6E879_7AC3_DB4A_41D0_A4C5A55A61B3.ok = OK ### Report Screen quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.title = - SCORE - quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.completion = Completed quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.questionsCorrect = Correct quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.downloadCSV = Download .csv quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.questionsIncorrect = Incorrect quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.items = Items Found quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.questions = Questions quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.repeat = Repeat quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.submitToLMS = Submit quizScore_6BF0C879_7AC3_DB4A_4185_E02580A618BF.elapsedTime = Time ### Score Name score1.label = Score 1 ### Timeout Screen quizTimeout_6BF79879_7AC3_DB4A_41DC_B9FEB819D849.title = - TIMEOUT - quizTimeout_6BF79879_7AC3_DB4A_41DC_B9FEB819D849.repeat = Repeat quizTimeout_6BF79879_7AC3_DB4A_41DC_B9FEB819D849.score = View Score ## Hotspot ### Text HotspotPanoramaOverlayTextImage_7321AFE6_BA09_9F14_41DC_6FB90E360F99.text = Instructions HotspotPanoramaOverlayTextImage_73222FE8_BA09_9F1C_41D6_BA3BE8D8DCA1.text = Introduction HotspotPanoramaOverlayTextImage_73223FE8_BA09_9F1C_41A5_38A951603BAE.text = Introduction HotspotPanoramaOverlayTextImage_73228FEB_BA09_9F1C_41C6_79C2CA3B5777.text = Introduction HotspotPanoramaOverlayTextImage_7322DFED_BA09_9F14_41A8_EDCF7A5E15B1.text = Introduction HotspotPanoramaOverlayTextImage_7322CFED_BA09_9F14_41D6_316B7C492274.text = Introduction HotspotPanoramaOverlayTextImage_7322BFEC_BA09_9F14_41CE_7D94D930E6ED.text = Introduction HotspotPanoramaOverlayTextImage_73229FEC_BA09_9F14_41AC_9801709339FF.text = Introduction HotspotPanoramaOverlayTextImage_73225FE9_BA09_9F1C_41E3_3EB4F7FAB1A2.text = Introduction HotspotPanoramaOverlayTextImage_7321FFE7_BA09_9F14_41DD_AFB8F1368C24.text = Introduction HotspotPanoramaOverlayTextImage_73220FE7_BA09_9F14_41DD_FCDDACE27BFA.text = Introduction HotspotPanoramaOverlayTextImage_73227FEA_BA09_9F1C_41E1_9CD5F279CA7E.text = Introduction HotspotPanoramaOverlayTextImage_73226FEA_BA09_9F1C_41DD_5E9F12DE56A0.text = Introduction HotspotPanoramaOverlayTextImage_73224FE9_BA09_9F1C_41D5_9215B8CBB923.text = Introduction HotspotPanoramaOverlayTextImage_73218FE5_BA09_9F14_41D7_42D4BDB2CC8D.text = Location 1 HotspotPanoramaOverlayTextImage_73214FE5_BA09_9F14_41CA_9767FFA744F5.text = Location 2 HotspotPanoramaOverlayTextImage_73219FE5_BA09_9F14_41D2_1578FBE4D741.text = Location 3 HotspotPanoramaOverlayTextImage_7321CFE6_BA09_9F14_41B7_02001E37B9AF.text = Location 4 HotspotPanoramaOverlayTextImage_7321EFE6_BA09_9F14_41E1_CF352A4EDAA4.text = Location 5 HotspotPanoramaOverlayTextImage_7321DFE6_BA09_9F14_41CE_03B976EEAE0C.text = Location 6 HotspotPanoramaOverlayTextImage_7321BFE6_BA09_9F14_41AE_753F4A282050.text = Location 7 HotspotPanoramaOverlayTextImage_73216FE5_BA09_9F14_41E1_98D49AFC5890.text = Location 8 ### Tooltip HotspotPanoramaOverlayArea_1D568756_8030_A250_41D6_4000BBFF5074.toolTip = 1.1.1 - Identifying and classifying rocks HotspotPanoramaOverlayArea_1FCAEA9E_8030_E2D0_41D9_FFC558A6097D.toolTip = 1.1.2 - Describing rocks HotspotPanoramaOverlayArea_165D1334_8031_E3D0_41B9_466975928317.toolTip = 1.1.3 - Interpreting field relationship HotspotPanoramaOverlayArea_15B37B1B_83CF_E3D0_41C9_10329F402660.toolTip = 1.1.4 - Describing rocks HotspotPanoramaOverlayArea_EA82E53C_A41B_38B0_41E3_C47A04D5334A.toolTip = 1.1.5 - Relative timing relationships HotspotPanoramaOverlayArea_EAF89514_A41B_3870_41E0_92432192A29A.toolTip = 1.1.6 - Interpreting field relationships HotspotPanoramaOverlayArea_1BB83470_9EC6_8540_41B5_F89DACFABEDB.toolTip = 1.2.1 - Interpreting how rocks formed HotspotPanoramaOverlayArea_1A739F66_9EC3_8340_41D2_2D947E199AEC.toolTip = 1.2.2 - Making a field map HotspotPanoramaOverlayArea_1C0F57DD_9EC5_8340_41DC_3AF9FC9E912A.toolTip = 1.2.3 - Plotting structural data onto a map HotspotPanoramaOverlayArea_EAF81283_A41B_5850_41DF_7A2FF3E62D21.toolTip = 1.2.4 - Interpreting how rock units formed HotspotPanoramaOverlayArea_EA89CBAE_A41B_2850_41C8_92AA4390ACF7.toolTip = 1.2.5 - Plotting and interpreting structural data on stereonets HotspotPanoramaOverlayArea_0972F36D_A1C3_8340_41A7_4F6178987520.toolTip = 1.3.1 - Petrographic description and interpretation HotspotPanoramaOverlayArea_0AB82927_A1C2_8CC0_41E1_C78375BFD789.toolTip = 1.3.2 - Integrating geochemistry HotspotPanoramaOverlayArea_0C85AB8C_A1C2_83C0_41DE_E52C968E0B60.toolTip = 1.3.3 - Integrating geochronology HotspotPanoramaOverlayArea_9E1685E5_A9B5_DA25_41D9_F13E0DA91B0B.toolTip = 2.1.1 - Rock description HotspotPanoramaOverlayArea_94AAD8CC_A994_EA6B_41D8_D16A5A0714AB.toolTip = 2.1.2 - Rock description HotspotPanoramaOverlayArea_EB88FF0F_AAAC_E7E5_41E4_DFF5217360F8.toolTip = 2.1.3 - Structural measurement HotspotPanoramaOverlayArea_EF813D68_AAAF_EA2B_41D5_90CC61CA487A.toolTip = 2.1.4 - Rock description HotspotPanoramaOverlayArea_C0BC3511_AB6D_FBFD_41D6_D9EB6B4E65A1.toolTip = 2.2.1 - Rock description HotspotPanoramaOverlayArea_C12FF623_AA93_B9DD_41C8_DF3CF6C5D755.toolTip = 2.2.2 - Rock description HotspotPanoramaOverlayArea_C1C0D823_AA93_E9DD_41C0_F1FE7BAA5270.toolTip = 2.2.3 - Structural identification HotspotPanoramaOverlayArea_C03B3938_AB6F_6A2B_41D6_AB1C941B2E4F.toolTip = 2.2.4 -Download structural data HotspotPanoramaOverlayArea_AE6048EC_B890_9583_41DB_F39BF554AA7C.toolTip = 2.3.1 - Rock description HotspotPanoramaOverlayArea_A2E516AE_B8B0_7D9F_41E4_E49212D02950.toolTip = 2.3.2 - Download the sedimentary log A - B HotspotPanoramaOverlayArea_9EBB6A9D_B970_95BD_4193_22F16A927ADA.toolTip = 2.3.3 - Download the sedimentary log C - D HotspotPanoramaOverlayArea_9EB11024_B970_F483_41D6_02CB84702980.toolTip = 2.3.4 - Rock description HotspotPanoramaOverlayArea_E0B2D912_B9F0_B487_41B4_A1E2C57BED68.toolTip = 3.1.1 - Rock description HotspotPanoramaOverlayArea_E47DBC3B_B9F1_8C85_41E3_91F0B6557EB2.toolTip = 3.1.2 - Rock description HotspotPanoramaOverlayArea_E79CA9D3_B9F0_F785_41B8_492F941AF7D4.toolTip = 3.1.3 - Rock description HotspotPanoramaOverlayArea_D5AE5709_B990_7C85_41C1_6B62A783B26F.toolTip = 3.2.1 - Structural measurement HotspotPanoramaOverlayArea_C55AB737_B991_BC8D_41B1_8B34193194AF.toolTip = 3.3.1 - Rock description HotspotPanoramaOverlayArea_C37CE49B_E1CA_8093_41D4_3A50014EF883.toolTip = 3.3.2 - Structural data to download and plot HotspotPanoramaOverlayArea_2E0985DD_B88F_9FBD_4198_3E55F0269557.toolTip = 4.1.1 - Rock description and classification HotspotPanoramaOverlayArea_FB1A3743_EC02_C9D9_41E7_159550180282.toolTip = 4.1.2 - Interpreting how rock units formed HotspotPanoramaOverlayArea_0F6C2FA7_BB90_8B8D_41E3_A853994D378A.toolTip = 4.1.3 - Rock description HotspotPanoramaOverlayArea_58AD9D18_BBB1_8C83_41C0_A331E0EF9F86.toolTip = 4.1.4 - Rock description and classification HotspotPanoramaOverlayArea_5A3EB64F_BB93_9C9D_41E7_9A0EEA8D163C.toolTip = 4.1.5 - Boundary identification HotspotPanoramaOverlayArea_62AB2AEC_BB91_9583_41D7_680040B06DF4.toolTip = 4.1.6 - Rock description and classification HotspotPanoramaOverlayArea_630F8B6E_BB90_949F_41E2_CD23D8B934AA.toolTip = 4.1.7 - Rock description and classification HotspotPanoramaOverlayArea_60ABE897_BB8F_958D_41B6_42ECBD3AA77E.toolTip = 4.1.8 - Field relationships among rack units HotspotPanoramaOverlayArea_617655CE_BB8F_9F9F_41D6_79A957ACD43A.toolTip = 4.1.9 - Rock description and classification HotspotPanoramaOverlayArea_4E4B38DF_BB93_95BD_41E4_F1127FF25207.toolTip = 4.2.1 - Interpreting how rock units formed HotspotPanoramaOverlayArea_4A496499_BB90_7D85_41E4_90CBE3FBDDA1.toolTip = 4.2.2 - Interpreting how rock units formed HotspotPanoramaOverlayArea_4A93B980_BB91_9783_41E4_6D629BB46C72.toolTip = 4.2.3 - Interpreting how rock units formed HotspotPanoramaOverlayArea_4B072A39_BB91_B485_41CA_C4B6198A75E0.toolTip = 4.2.4 - Interpreting how rock units formed HotspotPanoramaOverlayArea_48586CC7_BB91_8D8D_41B4_D622C35972ED.toolTip = 4.2.5 - Plotting structural data to download and plot HotspotPanoramaOverlayArea_4885DA99_BB91_9585_41E4_83C9DED533F6.toolTip = 4.2.6 - Interpreting how rock units formed HotspotPanoramaOverlayArea_514451D7_BB90_B78D_41E6_FE5972A788C6.toolTip = 4.2.7 - Interpreting how rock units formed HotspotPanoramaOverlayArea_496A1C32_BB90_8C87_41C1_8C390A828CE6.toolTip = 4.2.8 - Interpreting how rock units formed HotspotPanoramaOverlayArea_BEA193F9_B8B3_9B85_41E4_61B4B301E4BE.toolTip = 4.3.1 - Petrographic description and interpretation HotspotPanoramaOverlayArea_BEA1F328_B8B3_9483_41B8_48587C26AA46.toolTip = 4.3.2 - Interpret geochemistry data in context of field relationships HotspotPanoramaOverlayArea_BE9F5FB6_B890_8B8F_41E3_7B82BECD8FF8.toolTip = 4.3.3 - Petrographic description and interpretation HotspotPanoramaOverlayArea_BE9FC428_B88F_FC83_41CC_C1BF81D13D4D.toolTip = 4.3.4 - Interpret geochemistry data in context of field relationships HotspotPanoramaOverlayArea_BEE2D240_B8B1_9483_41E5_5FDF782056B5.toolTip = 5.1.1 - Relative timing HotspotPanoramaOverlayArea_BEE2EA76_B8B1_B48F_41A3_185CFF76E7A9.toolTip = 5.1.2 - Rock description video HotspotPanoramaOverlayArea_BEE50F5F_B8B0_8CBD_41CB_38BBF05464CC.toolTip = 5.1.3 - Structural measurements HotspotPanoramaOverlayArea_BF09033B_B970_7485_41E3_22FC80EC646B.toolTip = 5.1.4 -Describing structures HotspotPanoramaOverlayArea_BF1A04B0_B990_7D83_41D1_B327353CF677.toolTip = 5.2.1 - Measuring elements of a fold video HotspotPanoramaOverlayArea_BF1A1E32_B990_8C87_41D4_4A49C76BE87C.toolTip = 5.2.2 - Describing fold elements in the field HotspotPanoramaOverlayArea_BF1A2CD7_B990_8D8D_41E0_EE3F98D6450B.toolTip = 5.2.3 - Structural data to download and plot HotspotPanoramaOverlayArea_BF1A3EB2_B990_8D87_41D2_A12C7E051767.toolTip = 5.2.4 - Measuring structures HotspotPanoramaOverlayArea_BF1A5671_B990_9C85_41E3_589501C247C0.toolTip = 5.2.5 - Measuring and classifying folds HotspotPanoramaOverlayArea_FCF50BD7_C36A_D4F9_41CD_D1BFD5911A0E.toolTip = 5.2.6 - Structural data to download and plot HotspotPanoramaOverlayArea_8806BAFD_C329_34A9_41D6_617504F2C225.toolTip = 5.2.7 - Measuring structures HotspotPanoramaOverlayArea_FC9043A8_C366_D557_41D6_A65FEE9E47F0.toolTip = 5.2.8 - Structural data to download and plot HotspotPanoramaOverlayArea_83B968C3_C359_74D9_41D5_ABED339FC6D5.toolTip = 5.2.9 - Making a map HotspotPanoramaOverlayArea_DD7A9C89_C3E9_7369_41C8_1128DE997378.toolTip = 5.3.1 - Old mine workings HotspotPanoramaOverlayArea_DD24AE10_C3E9_2F77_41E5_3641DF23BB80.toolTip = 5.3.2 - Describing fold elements in the field HotspotPanoramaOverlayArea_DD186029_C3E9_53A9_41E5_E349F15745D8.toolTip = 5.3.3 - Measuring elements of a fold HotspotPanoramaOverlayArea_F58F0414_C369_337F_41E5_F0B0BAB2F131.toolTip = 5.3.4 - Interpretation of formation HotspotPanoramaOverlayArea_A3B5CD97_C56F_ED79_41D4_08E4A73D6F05.toolTip = 6.1.1 - Making geological sketches of rocks and their relationships HotspotPanoramaOverlayArea_EECFE5F3_CBFC_7BAC_41E8_5A2C74699F11.toolTip = 6.1.1 - download: drone photography of pillow basalt HotspotPanoramaOverlayArea_A3C12EA9_C56F_2CA9_41B2_F6EA6A046CB2.toolTip = 6.1.2 - Interpreting how rock units formed \ HotspotPanoramaOverlayArea_AC5C11D8_C56F_54E8_41A1_B3D77D22FD94.toolTip = 6.2.1 - Interpreting how rock units formed HotspotPanoramaOverlayArea_ACC6C3A2_C56E_D55B_41D5_018063B9F424.toolTip = 6.3.1 - Incorporating micro-scope-scale observation HotspotPanoramaOverlayArea_AD1B181B_C56E_F369_41D8_F1397F603736.toolTip = 6.3.2 - Interpret geochemistry data in context of field relationships HotspotPanoramaOverlayArea_A2025CF0_CD94_A9AC_41DB_C37032C0AD9B.toolTip = 7.1.1 - Identify and classifying rocks based on descriptions HotspotPanoramaOverlayArea_A2B990CA_CD94_99FC_41CD_D8F9A97701D7.toolTip = 7.1.2 - Identify and classifying rocks based on descriptions \ HotspotPanoramaOverlayArea_A28F9349_CD94_F8FC_41DC_2D4F16741916.toolTip = 7.1.3 - Identify and classifying rocks based on descriptions HotspotPanoramaOverlayArea_A5252253_CD94_98EC_41B2_297448044036.toolTip = 7.2.1 - Geological history from field observations HotspotPanoramaOverlayArea_A5EDC5DD_CD94_7B94_41E8_C450BA5C134E.toolTip = 7.2.2 - Interpreting relationships from a field map HotspotPanoramaOverlayArea_A5A41144_CD95_B8F4_41CB_35A01D25EAFA.toolTip = 7.3.1 - Incorporating micro-scope-scale observation HotspotPanoramaOverlayArea_A45C358D_CD95_9874_419B_F9142DFC1B2A.toolTip = 7.3.2 - Incorporating micro-scope-scale observation HotspotPanoramaOverlayArea_A427F6CD_CD95_F9F4_41DB_CA3052A1F3A6.toolTip = 7.3.3 - Interpret geochemistry data in context of field relationships HotspotPanoramaOverlayArea_2CD60D48_C4F4_68FC_4168_A84D49EE55E4.toolTip = 8.1.1 - Describing rocks using various criteria HotspotPanoramaOverlayArea_2FC7CBEB_C4F7_AFBC_41D9_E444FAB71A1A.toolTip = 8.1.2 - Describing rocks using various criteria HotspotPanoramaOverlayArea_2EFF9C15_C4F7_A894_41E4_2C41CC537616.toolTip = 8.2.1 - Interpreting how rocks units are formed HotspotPanoramaOverlayArea_2E13F7ED_C4F4_67B4_41D6_C561EE5A6B77.toolTip = 8.2.2 - Showing geological relationships using appropriate map symbols HotspotPanoramaOverlayArea_29564D6E_C4F4_A8B4_41E6_11BEDDE2D731.toolTip = 8.3.1 - Interpret geochemistry data in context of field relationships HotspotPanoramaOverlayArea_E820F011_EE4B_9F6F_41E8_DE985078E440.toolTip = Go to location 1 HotspotPanoramaOverlayArea_E8116132_EE4A_81AD_41DF_1A71A1732D08.toolTip = Go to location 2 HotspotPanoramaOverlayArea_72C25AE7_EC01_F8D9_41E3_5AB298EE01B3.toolTip = Go to location 3 HotspotPanoramaOverlayArea_92F46192_EC01_C97B_41ED_186E85A09822.toolTip = Go to location 4 HotspotPanoramaOverlayArea_6A59EFC5_EC03_78D9_41E0_65C971F8F1E1.toolTip = Go to location 5 HotspotPanoramaOverlayArea_F29D04A4_F403_4F5F_41EC_4C1E6BEA67A3.toolTip = Go to location 6 HotspotPanoramaOverlayArea_910BD8C3_EC06_D8D9_41DC_DB9307C60F67.toolTip = Go to location 7 HotspotPanoramaOverlayArea_E81FB42E_EE75_87B5_41D3_A6579694984B.toolTip = Go to location 8 HotspotPanoramaOverlayArea_9798E99A_A4ED_6870_41CA_2AADFFFBD4FA.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_833EF918_A42D_2870_41A7_15228A1A6924.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_EA73CE1F_A417_2870_41E3_ABDCB71E1125.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_9078F7EE_A4ED_67D0_41D0_FF29DEA248ED.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_97E38CFB_A4ED_29B0_41D8_402F02AFF149.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_EAE235A9_A415_D850_41D2_2D813D386512.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_90A3D881_A4EB_2850_41DE_EA5ACE5FDB87.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_97BA2C62_A4EC_E8D0_41C4_1A48A0895895.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_82E5340B_A42D_7850_41D9_1812B0B0E8B9.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_914E0CD1_A4F5_29F0_41DE_31396389D48E.toolTip = Go to next panorama at this location HotspotPanoramaOverlayArea_EF0EE8F9_AA94_AA2D_41E1_9642580CB62F.toolTip = Introduction video HotspotPanoramaOverlayArea_BED0A944_B891_B483_41E4_6C671922CAC7.toolTip = Introduction video HotspotPanoramaOverlayArea_EA73CF85_B9F3_8B8D_41DB_9C0260FC82BB.toolTip = Introduction video HotspotPanoramaOverlayArea_CB40D08E_AA9D_BAE7_41E4_0E081AE47C88.toolTip = Introduction video HotspotPanoramaOverlayArea_BED09134_B891_9483_41D9_9A755B971E0F.toolTip = Introduction video HotspotPanoramaOverlayArea_BED01C0D_B890_8C9D_41DE_E0F90EC63DFC.toolTip = Introduction video HotspotPanoramaOverlayArea_BED167E4_B890_BB83_41D2_471B9C23B73D.toolTip = Introduction video HotspotPanoramaOverlayArea_BED1801E_B890_74BF_41E1_DA647E6A54A9.toolTip = Introduction video HotspotPanoramaOverlayArea_EA2D3038_B9F0_9483_41DD_E79D4123B160.toolTip = Introduction video HotspotPanoramaOverlayArea_8991A1D3_A9F4_BA7D_41E0_629ED58A5661.toolTip = Introduction video 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htmlText_F81DFF31_A402_EF22_41B8_B729D1736D7B.html =


htmlText_F81DFF31_A402_EF22_41B8_B729D1736D7B.html =


htmlText_295A7D80_C4F4_A86C_41DB_380656ADE410.html =
Correct. The data plot along a trend from N-MORB, suggesting some crustal contamination.
htmlText_4A4D64DD_BB90_7DBD_41E5_439AEB9D83BF.html =
Correct, the answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_29552D81_C4F4_A86C_41D2_015013D09CF4.html =
Incorrect. The data do not plot on the volcanic arc array.
htmlText_295ADD7D_C4F4_A894_41E1_1BE52FBCF5EF.html =
Incorrect. The data plot away from an OIB source.
htmlText_295ACD7F_C4F4_A894_41E8_52AB22FB8C02.html =
Incorrect. The data plot along a trend from N-MORB, suggesting some crustal contamination.
htmlText_4E7958EE_BB93_959F_41DA_79D821115275.html =
Not correct, the answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4A4C64DE_BB90_7DBF_41E7_6CC053DBF14A.html =
Not correct, the answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4A4DB4DA_BB90_7D87_41D6_62F777DAE914.html =
Not correct, the answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4A4D24DB_BB90_7D85_41A1_E845AB78AEF1.html =
Not correct, the answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_7C49977F_AC02_BF1E_41DD_F5958E25F806.html =
A fault is the structure that is responsible for truncating layers in this location.
htmlText_DCDA28F4_A403_7122_41DD_7B59C784ED6F.html =
All the answers are correct.
htmlText_0031E04F_AC02_917E_41D3_29AE7EE07611.html =
Basalt is the correct answer.
Rock types, rhyolite and dacite are darker than basalt and dolerite is a fine-grained rock type.
htmlText_2CE7CD5D_C4F4_6894_41D8_0E90D380A968.html =
Incorrect. Pillows in this location are 30-60 cm across.
htmlText_2CE7BD5E_C4F4_6894_41DA_F201E20357C4.html =
Incorrect. Pillows in this location are 30-60 cm across.
htmlText_2CE46D5C_C4F4_6894_41C2_09FF16A8C8EA.html =
Incorrect. Pillows in this location are 30-60 cm across.
htmlText_04AE874A_AC0E_9F66_41E3_9AE0B416BC64.html =
Pegmatitic gabbro is the correct answer and is the most suitable field name.
The rock type gabbro is grabbo but pegmatitic gabbro is more suitable. Dolerite is a medium mafic rock and basil is a fine grained mafic rock.
htmlText_04AE874A_AC0E_9F66_41E3_9AE0B416BC64.html =
Pegmatitic gabbro is the correct answer and is the most suitable field name.
The rock type gabbro is grabbo but pegmatitic gabbro is more suitable. Dolerite is a medium mafic rock and basil is a fine grained mafic rock.
htmlText_04AE874A_AC0E_9F66_41E3_9AE0B416BC64.html =
Pegmatitic gabbro is the correct answer and is the most suitable field name.
The rock type gabbro is grabbo but pegmatitic gabbro is more suitable. Dolerite is a medium mafic rock and basil is a fine grained mafic rock.
htmlText_04AE874A_AC0E_9F66_41E3_9AE0B416BC64.html =
Pegmatitic gabbro is the correct answer and is the most suitable field name.
The rock type gabbro is grabbo but pegmatitic gabbro is more suitable. Dolerite is a medium mafic rock and basil is a fine grained mafic rock.
htmlText_07EBD39F_AC06_B71E_41DD_B6B5BBA1415E.html =
Pyroxenite and gabbro and intruded an earlier basalt flow and basalt, pyroxenite and gabbro are different parts of a differentiated flow are consistent with observations and can be tested by field mapping.
Basalt forms a chilled margin of a pyroxenite intrusion is not consisent with your findings from the three rock types in this locality. A chilled margin of a pyroxenite should also be ultramafic.
Basalt lava flow was extruded over pyroxenite this is easible, this would require a period of erosion before a basalt flow and is not the simplest explanation.
htmlText_06407037_AC0E_B12E_41D1_9B05D42ACD5E.html =
Silica and total alkali composition of pegmatitic gabbro sample MH58 compare to other mafic rocks in the area and are not significantly distinguishable.
MH58 has a similar SiO2 and total alkali content.
htmlText_D255202A_A403_B126_41DB_958E23B130CC.html =
The answer is: MH15, MH14, MH20, MH55, MH56.
htmlText_2CE44D5D_C4F4_6894_41C4_C551051F831A.html =
The correct answer is: 30-60 cm across.
htmlText_DB673344_A403_9762_41C6_9347203A2F77.html =
The felsic dyke cross cut the foliation and therefore the dyke is younger than the tectonic foliation.
htmlText_DB673344_A403_9762_41C6_9347203A2F77.html =
The felsic dyke cross cut the foliation and therefore the dyke is younger than the tectonic foliation.
htmlText_1B41140F_AC06_B0FE_41D3_2ADEBE190C34.html =
The tectonic environment would be compatible with the presence of pillow lava are:
- a mid-ocean ridge at a divergent plate boundary
- a back-arc basin
- plume-related ocean island volcanism
htmlText_1B41140F_AC06_B0FE_41D3_2ADEBE190C34.html =
The tectonic environment would be compatible with the presence of pillow lava are:
- a mid-ocean ridge at a divergent plate boundary
- a back-arc basin
- plume-related ocean island volcanism
htmlText_293FADF0_A47D_9322_41CC_2320105FAEDA.html =
A microscopic spinifex texture indicates supercooling of melt.
htmlText_E97621FA_A402_9326_41D2_C9F5D433F1EE.html =
Although slightly variable, overall, the contract trends NE-SW.
htmlText_E97621FA_A402_9326_41D2_C9F5D433F1EE.html =
Although slightly variable, overall, the contract trends NE-SW.
htmlText_0DDA2582_AC02_F3E6_41E5_0E4449026C52.html =
An igneous rock with this grain size is pegmatitic.
htmlText_0DDA2582_AC02_F3E6_41E5_0E4449026C52.html =
An igneous rock with this grain size is pegmatitic.
htmlText_EF4C1E17_A40D_B0EE_41E3_71F9D7765711.html =
Dykes open parallel to the least compressive stress (sigma 3) direction. Here, sigma 3 much be ESE-WNW – perpendicular to the dyke margin.
htmlText_2AA88E3D_A407_9122_4184_5447B29E26FB.html =
Each variole has a radiating pattern of crystals, indicating radial growth from the variole cores.
htmlText_2AA88E3D_A407_9122_4184_5447B29E26FB.html =
Each variole has a radiating pattern of crystals, indicating radial growth from the variole cores.
htmlText_2AA88E3D_A407_9122_4184_5447B29E26FB.html =
Each variole has a radiating pattern of crystals, indicating radial growth from the variole cores.
htmlText_2AA88E3D_A407_9122_4184_5447B29E26FB.html =
Each variole has a radiating pattern of crystals, indicating radial growth from the variole cores.
htmlText_EBFABDE9_A405_7322_41C3_9CC982338574.html =
Even though the data indicate the zircon grains have lost Pb (recent) and have common Pb contamination (all to be expected in the Yilgarn Craton), the seven most concordant points yield ~2673 Ma, which is the best estimate of magmatic.
htmlText_EBFABDE9_A405_7322_41C3_9CC982338574.html =
Even though the data indicate the zircon grains have lost Pb (recent) and have common Pb contamination (all to be expected in the Yilgarn Craton), the seven most concordant points yield ~2673 Ma, which is the best estimate of magmatic.
htmlText_EBFABDE9_A405_7322_41C3_9CC982338574.html =
Even though the data indicate the zircon grains have lost Pb (recent) and have common Pb contamination (all to be expected in the Yilgarn Craton), the seven most concordant points yield ~2673 Ma, which is the best estimate of magmatic.
htmlText_EBFABDE9_A405_7322_41C3_9CC982338574.html =
Even though the data indicate the zircon grains have lost Pb (recent) and have common Pb contamination (all to be expected in the Yilgarn Craton), the seven most concordant points yield ~2673 Ma, which is the best estimate of magmatic.
htmlText_E6E9C125_A402_9322_41E2_F859EA618F68.html =
For strike slip faults, sigma 2 is vertical, and sigma 1 and sigma 3 are oriented obliquely to the fault plane.
htmlText_E8FDAE65_A405_9122_41CD_F89DB336FC85.html =
Ideally, weighted mean ages have an MSWD = 1 and p = 1. The values of 0.65 and 0.69 are acceptable close to 1.
htmlText_E8FDAE65_A405_9122_41CD_F89DB336FC85.html =
Ideally, weighted mean ages have an MSWD = 1 and p = 1. The values of 0.65 and 0.69 are acceptable close to 1.
htmlText_2DD539A5_A41D_7322_41B0_B1DB14D08DFC.html =
Inflation of pillows causes quenching of a layered glassy skin when in contact with water.
htmlText_2DD539A5_A41D_7322_41B0_B1DB14D08DFC.html =
Inflation of pillows causes quenching of a layered glassy skin when in contact with water.
htmlText_F8F891C4_A403_B362_41BF_DBB8B26EDEE9.html =
It requires flow to form an erosive base.
htmlText_E5DD9DC7_A402_936E_41D7_EEAF852CA314.html =
Light REE becomes enriched in the melt by fractional crystallization because they are incompatible in most magmatic silicate phases.
htmlText_E5DD9DC7_A402_936E_41D7_EEAF852CA314.html =
Light REE becomes enriched in the melt by fractional crystallization because they are incompatible in most magmatic silicate phases.
htmlText_E5DD9DC7_A402_936E_41D7_EEAF852CA314.html =
Light REE becomes enriched in the melt by fractional crystallization because they are incompatible in most magmatic silicate phases.
htmlText_E5DD9DC7_A402_936E_41D7_EEAF852CA314.html =
Light REE becomes enriched in the melt by fractional crystallization because they are incompatible in most magmatic silicate phases.
htmlText_E5DD9DC7_A402_936E_41D7_EEAF852CA314.html =
Light REE becomes enriched in the melt by fractional crystallization because they are incompatible in most magmatic silicate phases.
htmlText_E5DD9DC7_A402_936E_41D7_EEAF852CA314.html =
Light REE becomes enriched in the melt by fractional crystallization because they are incompatible in most magmatic silicate phases.
htmlText_E5DD9DC7_A402_936E_41D7_EEAF852CA314.html =
Light REE becomes enriched in the melt by fractional crystallization because they are incompatible in most magmatic silicate phases.
htmlText_E5DD9DC7_A402_936E_41D7_EEAF852CA314.html =
Light REE becomes enriched in the melt by fractional crystallization because they are incompatible in most magmatic silicate phases.
htmlText_2FCB7C01_C4F7_A86C_41DA_757C5F2BEB1B.html =
Pillows young towards the west.
htmlText_2FCACBFF_C4F7_AF94_41E5_C7E58B21C503.html =
Pillows young towards the west.
htmlText_2FCAFC00_C4F7_A86C_418D_F681D7BFB780.html =
Pillows young towards the west.
htmlText_2FCB9C02_C4F7_A86C_41B7_B14322E4808A.html =
Pillows young towards the west.
htmlText_2E17BEBF_A402_F11E_41DF_A6B3EDBE41E3.html =
Radiating crystals and indistinct margins are consistent with devitrification of volcanic glass.
htmlText_2E17BEBF_A402_F11E_41DF_A6B3EDBE41E3.html =
Radiating crystals and indistinct margins are consistent with devitrification of volcanic glass.
htmlText_2E17BEBF_A402_F11E_41DF_A6B3EDBE41E3.html =
Radiating crystals and indistinct margins are consistent with devitrification of volcanic glass.
htmlText_2E17BEBF_A402_F11E_41DF_A6B3EDBE41E3.html =
Radiating crystals and indistinct margins are consistent with devitrification of volcanic glass.
htmlText_2E17BEBF_A402_F11E_41DF_A6B3EDBE41E3.html =
Radiating crystals and indistinct margins are consistent with devitrification of volcanic glass.
htmlText_2E17BEBF_A402_F11E_41DF_A6B3EDBE41E3.html =
Radiating crystals and indistinct margins are consistent with devitrification of volcanic glass.
htmlText_2E17BEBF_A402_F11E_41DF_A6B3EDBE41E3.html =
Radiating crystals and indistinct margins are consistent with devitrification of volcanic glass.
htmlText_2E17BEBF_A402_F11E_41DF_A6B3EDBE41E3.html =
Radiating crystals and indistinct margins are consistent with devitrification of volcanic glass.
htmlText_7F15E9A6_AC05_B32E_41D5_C5789AEA4215.html =
Sequence the samples from the least evolved to the most evolved are:
MH15, MH14, MH20, MH55, MH56
htmlText_7F15E9A6_AC05_B32E_41D5_C5789AEA4215.html =
Sequence the samples from the least evolved to the most evolved are:
MH15, MH14, MH20, MH55, MH56
htmlText_C4B584D8_A406_F162_41CB_04671C440C4F.html =
The answer 87 degrees northeast.
htmlText_C4B584D8_A406_F162_41CB_04671C440C4F.html =
The answer 87 degrees northeast.
htmlText_DDBCE9D4_A402_F362_41DF_9C58897174F1.html =
The answer is sedimentary layers deposited, then folded and foliated, then intruded by a felsic dyke.
htmlText_FE8AEDDA_A403_7366_41D2_F6EF4D94FBFA.html =
The answer is 156 or 336.
htmlText_C2ECDD2F_A407_933E_419B_D7A2040970FC.html =
The answer is 43 degrees NE.
htmlText_C2ECDD2F_A407_933E_419B_D7A2040970FC.html =
The answer is 43 degrees NE.
htmlText_2FAE61C5_A403_9362_41DF_3E23E776C2AC.html =
The answer is 60%.
htmlText_DC0ECEBE_A402_F11E_41BA_20956D61AF94.html =
The answer is NW - SE.
htmlText_D3D3AD72_A403_7326_41DB_6C1A5A400CA8.html =
The answer is NW-SE.
htmlText_C2F59DA1_A402_F322_4193_6CD44593DA3E.html =
The answer is NW-SE.
htmlText_C1DC8AAC_A40D_7122_41A3_6DECC29E1E39.html =
The answer is NW-SE.
htmlText_D0AE4394_A41E_97E2_41E2_7C21486207B9.html =
The answer is basalt.
htmlText_D1C69201_A406_90E2_41E3_00F2C12D3DFF.html =
The answer is clinopyroxene.
htmlText_DD59B40A_A40D_70E6_41D4_D150F2FF8303.html =
The answer is close.
htmlText_DD59B40A_A40D_70E6_41D4_D150F2FF8303.html =
The answer is close.
htmlText_DD59B40A_A40D_70E6_41D4_D150F2FF8303.html =
The answer is close.
htmlText_DD59B40A_A40D_70E6_41D4_D150F2FF8303.html =
The answer is close.
htmlText_DD59B40A_A40D_70E6_41D4_D150F2FF8303.html =
The answer is close.
htmlText_DD59B40A_A40D_70E6_41D4_D150F2FF8303.html =
The answer is close.
htmlText_DD59B40A_A40D_70E6_41D4_D150F2FF8303.html =
The answer is close.
htmlText_DD59B40A_A40D_70E6_41D4_D150F2FF8303.html =
The answer is close.
htmlText_DDA2C619_A41E_90E2_41D3_AC280065639A.html =
The answer is dolerite.
htmlText_D277DF50_A405_6F62_41E3_6953C0B9A6DC.html =
The answer is felsic porphyry.
htmlText_D277DF50_A405_6F62_41E3_6953C0B9A6DC.html =
The answer is felsic porphyry.
htmlText_D277DF50_A405_6F62_41E3_6953C0B9A6DC.html =
The answer is felsic porphyry.
htmlText_D277DF50_A405_6F62_41E3_6953C0B9A6DC.html =
The answer is felsic porphyry.
htmlText_D277DF50_A405_6F62_41E3_6953C0B9A6DC.html =
The answer is felsic porphyry.
htmlText_D277DF50_A405_6F62_41E3_6953C0B9A6DC.html =
The answer is felsic porphyry.
htmlText_D277DF50_A405_6F62_41E3_6953C0B9A6DC.html =
The answer is felsic porphyry.
htmlText_D277DF50_A405_6F62_41E3_6953C0B9A6DC.html =
The answer is felsic porphyry.
htmlText_FFC67BA9_A43D_F722_41D6_B44B1324D3E9.html =
The answer is fine grained felsic.
htmlText_C40FC27B_A402_9126_41C6_77B0653CC445.html =
The answer is flattening due to compaction in a hot volcanic ash flow.
htmlText_C40FC27B_A402_9126_41C6_77B0653CC445.html =
The answer is flattening due to compaction in a hot volcanic ash flow.
htmlText_D1251F47_A40F_EF6E_41D7_FEF3C49666F5.html =
The answer is interstitial.
htmlText_D1251F47_A40F_EF6E_41D7_FEF3C49666F5.html =
The answer is interstitial.
htmlText_41DDC3AE_BA19_8714_41CA_E478A6A7A64C.html =
The answer is mafic.
htmlText_D10E5EA6_A402_912E_41DB_88FC5311D2B9.html =
The answer is orthopyroxene.
htmlText_D10E5EA6_A402_912E_41DB_88FC5311D2B9.html =
The answer is orthopyroxene.
htmlText_D12A53FE_A406_F71E_41E2_DB609583CB8F.html =
The answer is plagioclase.
htmlText_D12E6BA3_A405_F726_41E0_A7F16CF69B84.html =
The answer is porphyritic.
htmlText_D12E6BA3_A405_F726_41E0_A7F16CF69B84.html =
The answer is porphyritic.
htmlText_D12E6BA3_A405_F726_41E0_A7F16CF69B84.html =
The answer is porphyritic.
htmlText_D12E6BA3_A405_F726_41E0_A7F16CF69B84.html =
The answer is porphyritic.
htmlText_DECC0387_A405_97EE_41BD_3E61085D1053.html =
The answer is porphyritic.
htmlText_DECC0387_A405_97EE_41BD_3E61085D1053.html =
The answer is porphyritic.
htmlText_DECC0387_A405_97EE_41BD_3E61085D1053.html =
The answer is porphyritic.
htmlText_DECC0387_A405_97EE_41BD_3E61085D1053.html =
The answer is porphyritic.
htmlText_DED071CB_A402_9366_41E0_E5EC79CFF92B.html =
The answer is spaced axial planar cleavage.
htmlText_D029BBB3_A402_9726_41D1_862C052D6293.html =
The answer is spinifex basalt.
htmlText_D029BBB3_A402_9726_41D1_862C052D6293.html =
The answer is spinifex basalt.
htmlText_DD01200C_A40F_90E2_41C5_967081097DFB.html =
The answer is spinifex.
htmlText_E59D053B_A405_9326_41D8_C0E54B695F2C.html =
The answer is strongly light-REE enriched.
htmlText_E59D053B_A405_9326_41D8_C0E54B695F2C.html =
The answer is strongly light-REE enriched.
htmlText_CDFAA165_A405_9322_41DB_17DA91B0362F.html =
The answer is tectonic deformation.
htmlText_2F9C7748_A40E_9F62_41D9_D89D853316C5.html =
The answer is the rock is rich in magnesium.
htmlText_DE7E9F35_A405_6F22_41C9_82C2EB508B75.html =
The answer is ultramafic.
htmlText_DE7E9F35_A405_6F22_41C9_82C2EB508B75.html =
The answer is ultramafic.
htmlText_DE7E9F35_A405_6F22_41C9_82C2EB508B75.html =
The answer is ultramafic.
htmlText_DE7E9F35_A405_6F22_41C9_82C2EB508B75.html =
The answer is ultramafic.
htmlText_DE7E9F35_A405_6F22_41C9_82C2EB508B75.html =
The answer is ultramafic.
htmlText_DE7E9F35_A405_6F22_41C9_82C2EB508B75.html =
The answer is ultramafic.
htmlText_DE7E9F35_A405_6F22_41C9_82C2EB508B75.html =
The answer is ultramafic.
htmlText_DE7E9F35_A405_6F22_41C9_82C2EB508B75.html =
The answer is ultramafic.
htmlText_DD1C01F2_A402_9326_41CF_4D0DBB94ECF3.html =
The answer is vertical.
htmlText_DD1C01F2_A402_9326_41CF_4D0DBB94ECF3.html =
The answer is vertical.
htmlText_DD1C01F2_A402_9326_41CF_4D0DBB94ECF3.html =
The answer is vertical.
htmlText_DEC7A855_A406_9162_41D1_186D01A3349C.html =
The answer is vertical.
htmlText_DD1C01F2_A402_9326_41CF_4D0DBB94ECF3.html =
The answer is vertical.
htmlText_DEC7A855_A406_9162_41D1_186D01A3349C.html =
The answer is vertical.
htmlText_2C3E4D34_A403_9322_41DA_2AA7959A51DF.html =
The answer is younging to the west.
htmlText_4B38AA4F_BB91_B49D_41D8_2E90B8C56C18.html =
The answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4A97599B_BB91_9785_41DF_FA4EB1818E27.html =
The answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4A96599C_BB91_9783_41E6_FF57FCF1952A.html =
The answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4B3B0A4E_BB91_B49F_41D4_EC7079B5414A.html =
The answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4A97E999_BB91_9785_41E6_C33883D76C36.html =
The answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4B383A51_BB91_B485_41CE_E16C7CC5482A.html =
The answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4B3BDA52_BB91_B487_41C8_4E5D1B068203.html =
The answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4A978997_BB91_978D_41D9_33368C7FBD4D.html =
The answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4E7938EF_BB93_959D_41E0_C9A6F97CA73B.html =
The answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_4E7898F0_BB93_9583_41C1_D72279BCEF9A.html =
The answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_D2B1A1BA_A43D_F326_41C7_966D61F92725.html =
The answer is a hyperbyssal intrusion.
htmlText_DE53FC43_A43F_9166_41D9_9ED01A60FD45.html =
The answer is folding involved layer-parallel shearing.
htmlText_DE53FC43_A43F_9166_41D9_9ED01A60FD45.html =
The answer is folding involved layer-parallel shearing.
htmlText_D32E5D9A_A40D_B3E6_41A0_E075922C8AE4.html =
The answer is it is felsic to intermediate in composition.
htmlText_D32E5D9A_A40D_B3E6_41A0_E075922C8AE4.html =
The answer is it is felsic to intermediate in composition.
htmlText_D146FF55_A405_AF62_41DC_A940EFEE482B.html =
The answer is massive, crystalline, medium grained, porphyritic.
htmlText_D146FF55_A405_AF62_41DC_A940EFEE482B.html =
The answer is massive, crystalline, medium grained, porphyritic.
htmlText_D146FF55_A405_AF62_41DC_A940EFEE482B.html =
The answer is massive, crystalline, medium grained, porphyritic.
htmlText_D146FF55_A405_AF62_41DC_A940EFEE482B.html =
The answer is massive, crystalline, medium grained, porphyritic.
htmlText_D3BA2289_A407_F1E2_41B2_F7621A80456B.html =
The answer is steeply dipping W.
htmlText_7C7F6198_AC7E_93E2_418C_B9F73187D10B.html =
The answer is they do not contain alkali-bearing minerals.
htmlText_2780A56F_A406_933E_41A8_960FE0408C45.html =
The answer is: NW – SE.
htmlText_25260B8B_A406_B7E6_41B0_BD2551CE4453.html =
The answer is: NW-SE.
htmlText_25260B8B_A406_B7E6_41B0_BD2551CE4453.html =
The answer is: NW-SE.
htmlText_DD638125_A406_F322_41B9_D70F8642584B.html =
The answer is: striking E-W, dipping steeply N.
htmlText_D056B6AC_A403_B122_41D1_AAB0DF657289.html =
The answer is: was extruded as lava that cooled rapidly.
htmlText_D86FFA01_A40E_90E2_41D6_68B4E79E7D39.html =
The answer is: focus on mapping rock types, ductile and brittle structures, and alteration, especially near known old workings.
htmlText_D86FFA01_A40E_90E2_41D6_68B4E79E7D39.html =
The answer is: focus on mapping rock types, ductile and brittle structures, and alteration, especially near known old workings.
htmlText_D095CFBF_A403_6F1E_41D8_BF432700E602.html =
The answer is MH55 has significantly depleted HREE and a stronger negative NB+Ta anomaly.
htmlText_D095CFBF_A403_6F1E_41D8_BF432700E602.html =
The answer is MH55 has significantly depleted HREE and a stronger negative NB+Ta anomaly.
htmlText_D03B37DF_A402_9F1E_41D9_F1986407F573.html =
The answer is N-S.
htmlText_29022501_A405_F0E2_41D8_30FB920BB3EB.html =
The answer is dark green, laminated.
htmlText_FDA517BD_A405_7F22_41A5_03380314C618.html =
The answer is finely laminated.
htmlText_FDA517BD_A405_7F22_41A5_03380314C618.html =
The answer is finely laminated.
htmlText_DC23C251_A402_B162_41CD_10AFB9EDF926.html =
The answer is foliated.
htmlText_DE646A11_A40E_90E2_41D9_3BAF9DE0F0B9.html =
The answer is garnet.
htmlText_DE646A11_A40E_90E2_41D9_3BAF9DE0F0B9.html =
The answer is garnet.
htmlText_DE646A11_A40E_90E2_41D9_3BAF9DE0F0B9.html =
The answer is garnet.
htmlText_DE646A11_A40E_90E2_41D9_3BAF9DE0F0B9.html =
The answer is garnet.
htmlText_DCF1F6B6_A403_712E_41B8_1D297602B50A.html =
The answer is plagioclase.
htmlText_D392C318_A41E_B0E2_41BE_95F4DF5B87AF.html =
The answer is porphyritic pyroxenite.
htmlText_D392C318_A41E_B0E2_41BE_95F4DF5B87AF.html =
The answer is porphyritic pyroxenite.
htmlText_D392C318_A41E_B0E2_41BE_95F4DF5B87AF.html =
The answer is porphyritic pyroxenite.
htmlText_D392C318_A41E_B0E2_41BE_95F4DF5B87AF.html =
The answer is porphyritic pyroxenite.
htmlText_D392C318_A41E_B0E2_41BE_95F4DF5B87AF.html =
The answer is porphyritic pyroxenite.
htmlText_D392C318_A41E_B0E2_41BE_95F4DF5B87AF.html =
The answer is porphyritic pyroxenite.
htmlText_D392C318_A41E_B0E2_41BE_95F4DF5B87AF.html =
The answer is porphyritic pyroxenite.
htmlText_D392C318_A41E_B0E2_41BE_95F4DF5B87AF.html =
The answer is porphyritic pyroxenite.
htmlText_D392C318_A41E_B0E2_41BE_95F4DF5B87AF.html =
The answer is porphyritic pyroxenite.
htmlText_D392C318_A41E_B0E2_41BE_95F4DF5B87AF.html =
The answer is porphyritic pyroxenite.
htmlText_D392C318_A41E_B0E2_41BE_95F4DF5B87AF.html =
The answer is porphyritic pyroxenite.
htmlText_D392C318_A41E_B0E2_41BE_95F4DF5B87AF.html =
The answer is porphyritic pyroxenite.
htmlText_D392C318_A41E_B0E2_41BE_95F4DF5B87AF.html =
The answer is porphyritic pyroxenite.
htmlText_D392C318_A41E_B0E2_41BE_95F4DF5B87AF.html =
The answer is porphyritic pyroxenite.
htmlText_D392C318_A41E_B0E2_41BE_95F4DF5B87AF.html =
The answer is porphyritic pyroxenite.
htmlText_D392C318_A41E_B0E2_41BE_95F4DF5B87AF.html =
The answer is porphyritic pyroxenite.
htmlText_D28BFC04_A4FF_F0E2_41DA_CBB27E7F41CF.html =
The answer is sub-vertical.
htmlText_D28BFC04_A4FF_F0E2_41DA_CBB27E7F41CF.html =
The answer is sub-vertical.
htmlText_D924E526_A407_932E_41DB_8D4D2502AC39.html =
The answer is tight.
htmlText_D924E526_A407_932E_41DB_8D4D2502AC39.html =
The answer is tight.
htmlText_D924E526_A407_932E_41DB_8D4D2502AC39.html =
The answer is tight.
htmlText_D924E526_A407_932E_41DB_8D4D2502AC39.html =
The answer is tight.
htmlText_DF117BA7_A43F_772E_41BB_4991A2B7B4F1.html =
The answer was extruded as lava that was supercooled from high temperatures.
htmlText_1908F4A3_AC02_9126_41D4_35EA3C35C4C5.html =
The bladed crystals with simple twins and third-order interference colours are clinopyroxene.
Olivine does not form twins and has second-order interference colours. Chlorite and actinolite do not have third-order interference colours.
htmlText_1908F4A3_AC02_9126_41D4_35EA3C35C4C5.html =
The bladed crystals with simple twins and third-order interference colours are clinopyroxene.
Olivine does not form twins and has second-order interference colours. Chlorite and actinolite do not have third-order interference colours.
htmlText_F5DD0392_A407_F7E6_41CB_FCEC29B15AA0.html =
The contact is sharp and curved.
htmlText_D8790BFA_A41E_B726_41CA_8F905E7B60BC.html =
The correct answer is 15 degrees.
htmlText_D8790BFA_A41E_B726_41CA_8F905E7B60BC.html =
The correct answer is 15 degrees.
htmlText_25EDCC78_A405_7122_41DE_42146D18A852.html =
The correct answer is N-S.
htmlText_1BBF5142_AC02_B367_41DD_257B34194FD0.html =
The correct answer is bladed and/or acicular.
htmlText_1E263FF6_AC3E_AF2E_41D3_4161424BE08C.html =
The correct answer is chlorite which has anomalous interference colours and is a common greenschist facies metamorphic mineral in mafic rocks.
Quartz and plagioclase have first-order interference colours and actinolite has second-order interference colours.
htmlText_1E263FF6_AC3E_AF2E_41D3_4161424BE08C.html =
The correct answer is chlorite which has anomalous interference colours and is a common greenschist facies metamorphic mineral in mafic rocks.
Quartz and plagioclase have first-order interference colours and actinolite has second-order interference colours.
htmlText_1E263FF6_AC3E_AF2E_41D3_4161424BE08C.html =
The correct answer is chlorite which has anomalous interference colours and is a common greenschist facies metamorphic mineral in mafic rocks.
Quartz and plagioclase have first-order interference colours and actinolite has second-order interference colours.
htmlText_1E263FF6_AC3E_AF2E_41D3_4161424BE08C.html =
The correct answer is chlorite which has anomalous interference colours and is a common greenschist facies metamorphic mineral in mafic rocks.
Quartz and plagioclase have first-order interference colours and actinolite has second-order interference colours.
htmlText_D195D028_A402_9122_41D0_1316E7AA8CA3.html =
The correct answer is observed.
htmlText_D195D028_A402_9122_41D0_1316E7AA8CA3.html =
The correct answer is observed.
htmlText_01A60438_AC02_9122_41E0_ED7014669848.html =
The correct answer is solid pyroxene crystals precipitated from a fractioning magma sank and accumulated.
htmlText_01A60438_AC02_9122_41E0_ED7014669848.html =
The correct answer is solid pyroxene crystals precipitated from a fractioning magma sank and accumulated.
htmlText_F8D2550E_A403_90FE_41CC_CE62D1486266.html =
The correct answer is the blue symbol.
htmlText_F8D2550E_A403_90FE_41CC_CE62D1486266.html =
The correct answer is the blue symbol.
htmlText_C1CEC947_A407_936E_41A6_F460A59DC1BD.html =
The correct answer is: ‘z’ folds.
htmlText_C1CEC947_A407_936E_41A6_F460A59DC1BD.html =
The correct answer is: ‘z’ folds.
htmlText_CC333F5A_A403_6F66_41BB_B79DE78BB07D.html =
The correct answer is 029.
htmlText_05D19728_AC02_9F22_41DA_E43B28437C31.html =
The correct answer is Pyroxene and is the best term to classify this rock type.
Peridotite also contains olivine.
Gabbro also contains plagioclase feldspar.
Dunite contains over 90% olivine.
htmlText_59DAE3E5_BA1A_8714_41C9_A58382DE76B2.html =
The crystal forms are cube-shaped and are therefore cubic.
htmlText_00326FB1_AC05_6F22_41DF_C0DF49650CBA.html =
The description that fits the trace element distribution relative to MORB for pegmatitic gabbro sample MH58 best is slightly enriched LREE and a negative Nb+Ta anomaly.
htmlText_00326FB1_AC05_6F22_41DF_C0DF49650CBA.html =
The description that fits the trace element distribution relative to MORB for pegmatitic gabbro sample MH58 best is slightly enriched LREE and a negative Nb+Ta anomaly.
htmlText_E87ACFE4_A403_AF22_41B3_AAD9047C685D.html =
The dyke discontinues into aligned segments arranged in an overlapping stepwise manner known as ‘an echelon’. Each segment narrows to a tip.
htmlText_E6FCBF19_A402_90E2_41DE_BB8C41D94380.html =
The dyke on the opposite side has moved to the left, which is sinistral, or left lateral displacement.
htmlText_E4C6AFDA_A405_6F66_41DC_8AEC701BF973.html =
The dyke segments are discontinuous and separated from one another, i.e., sharply truncated and offset.
htmlText_E4C6AFDA_A405_6F66_41DC_8AEC701BF973.html =
The dyke segments are discontinuous and separated from one another, i.e., sharply truncated and offset.
htmlText_15ADBEB0_AC1E_9122_41D0_9A926976A0F9.html =
The environment that can be interpreted from the presence of pillow structures are:
Pillow lavas are most commonly associated with subaqueous extrusion and extrusion of lava over land (subaerial) however this is less common than a subaqueous extrusion origin.
htmlText_E521B855_A40D_7162_41C9_6DF27DF02F30.html =
The extraction of melt from a garnet-rich source region leads to the depleted heavy REE in the melt when the garnet remains in the source region.
htmlText_E521B855_A40D_7162_41C9_6DF27DF02F30.html =
The extraction of melt from a garnet-rich source region leads to the depleted heavy REE in the melt when the garnet remains in the source region.
htmlText_E521B855_A40D_7162_41C9_6DF27DF02F30.html =
The extraction of melt from a garnet-rich source region leads to the depleted heavy REE in the melt when the garnet remains in the source region.
htmlText_E521B855_A40D_7162_41C9_6DF27DF02F30.html =
The extraction of melt from a garnet-rich source region leads to the depleted heavy REE in the melt when the garnet remains in the source region.
htmlText_049725E2_AC02_B326_41D7_1EA742CBC07A.html =
The former pyroxene grains form a cumulate texture.
htmlText_0642095C_AC07_9362_41E3_60E23015466C.html =
The fracture surface is smooth and conchoidal.
htmlText_0642095C_AC07_9362_41E3_60E23015466C.html =
The fracture surface is smooth and conchoidal.
htmlText_A5E1C5F1_CD94_7BAC_41E6_E951C9C36865.html =
The interpretations can be made from field relationships among rock types shown on the map of location 7 are that
pyroxenite and gabbro both cross cut basalt.
htmlText_A5E185F2_CD94_7BAC_41C8_FC0518AE8671.html =
The interpretations can be made from field relationships among rock types shown on the map of location 7 are that
pyroxenite and gabbro both cross cut basalt.
htmlText_A5E6D5F3_CD94_7BAC_41E6_A0DBC390247D.html =
The interpretations can be made from field relationships among rock types shown on the map of location 7 are that
pyroxenite and gabbro both cross cut basalt.
htmlText_A5E055F0_CD94_7BAC_41E6_96DA9DAEF50C.html =
The interpretations can be made from field relationships among rock types shown on the map of location 7 are that
pyroxenite and gabbro both cross cut basalt.
htmlText_60075DCD_AC02_B362_41D1_794F8DA203A1.html =
The mineral clast under the hand lens is a quartz.
htmlText_60075DCD_AC02_B362_41D1_794F8DA203A1.html =
The mineral clast under the hand lens is a quartz.
htmlText_517A6CCD_BA17_8114_41E2_5D32DD0590C9.html =
The mineral is pyrite.
htmlText_517A6CCD_BA17_8114_41E2_5D32DD0590C9.html =
The mineral is pyrite.
htmlText_2D2121FB_A406_9326_41E4_6D03295B299D.html =
The predominantly contain more feldspar and less mafic minerals.
htmlText_2D2121FB_A406_9326_41E4_6D03295B299D.html =
The predominantly contain more feldspar and less mafic minerals.
htmlText_EA859E2D_A40D_9122_41D7_AED7A45D05E5.html =
The recent Pb-loss causes data points to shift to the right and contamination of common Pb shifts data points towards the common Pb isotopic composition in the top left. Data distribution indicated that zircon from this rock has been variably affected by both of these processes.
htmlText_CC9C0ED3_A405_9166_41B7_70A7B4336027.html =
The red symbol is the correct answer.
htmlText_00BF8A9C_AC07_91E2_41E4_A91AA5A0B266.html =
The rock is classified as mafic.
Felsic and intermediate rocks contain much less mafic materials. Ultramafic rocks contain much less plagioclase.
htmlText_4A9255D7_AC1D_B36E_41AB_0E2D89918729.html =
The translucent grey mineral clast has a hexagonal shape and is resistant to weathering is quartz.
htmlText_4A9255D7_AC1D_B36E_41AB_0E2D89918729.html =
The translucent grey mineral clast has a hexagonal shape and is resistant to weathering is quartz.
htmlText_4A9255D7_AC1D_B36E_41AB_0E2D89918729.html =
The translucent grey mineral clast has a hexagonal shape and is resistant to weathering is quartz.
htmlText_4A9255D7_AC1D_B36E_41AB_0E2D89918729.html =
The translucent grey mineral clast has a hexagonal shape and is resistant to weathering is quartz.
htmlText_7ECBD06E_AC07_F13E_41CA_105934C02451.html =
The trend of this structure is NW-SE.
htmlText_7ECBD06E_AC07_F13E_41CA_105934C02451.html =
The trend of this structure is NW-SE.
htmlText_33B87CD2_A402_9166_41D5_90ACA561C783.html =
The variolitic sample has a similar trace element distribution to other mafic rocks in the area.
htmlText_3699A0C7_A47D_716E_41DF_B380DAC1998E.html =
Their irregular and indistinct margins suggest they were formed by alteration rather than as primary objects.
htmlText_3699A0C7_A47D_716E_41DF_B380DAC1998E.html =
Their irregular and indistinct margins suggest they were formed by alteration rather than as primary objects.
htmlText_E677F28D_A41F_91E2_41D2_4B3E3AFABC4D.html =
These rocks plot in dacite and trachyte fields, and across the trends for both sub-alkaline and alkaline series.
htmlText_FC4F4209_A40D_70E2_41E4_17F1EE14D915.html =
They are felsic.
htmlText_2A9B31B2_A406_9326_41E2_BED80C66F7F4.html =
To test this hypothesis, other geochemical signatures of sedimentary input could be examined.
htmlText_2A9B31B2_A406_9326_41E2_BED80C66F7F4.html =
To test this hypothesis, other geochemical signatures of sedimentary input could be examined.
htmlText_8927F518_9B61_D797_417F_9183DBEAB30A.html =
Instructions:
These photos of several felsic dykes exposed within 300 m of this location.
Step 1
In a notebook, describe the mineralogy and texture of each sample, particularly the phenocryst, noting any similarities and/or differences.
Step 2
Make interpretations about the cooling history of these rocks.
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Instructions
These optical photomicrographs are from several porphyritic felsic dykes exposed within 300 m of this location.
Step 1
In a notebook, make petrographic descriptions of each sample, including mineralogy and texture of the groundmass and phenocrysts.
Step 2
Make interpretations about magnetic history, noting any possible petrogenetic links between the dykes.
htmlText_D26559F9_A43F_7322_419C_5CB02E6F54A1.html =
The answer is clinopyroxene.
htmlText_D39EA163_A47D_B326_41CA_83A6BA138E24.html =
The answer is porphyritic dolerite.
htmlText_D39EA163_A47D_B326_41CA_83A6BA138E24.html =
The answer is porphyritic dolerite.
htmlText_D39EA163_A47D_B326_41CA_83A6BA138E24.html =
The answer is porphyritic dolerite.
htmlText_D39EA163_A47D_B326_41CA_83A6BA138E24.html =
The answer is porphyritic dolerite.
htmlText_D39EA163_A47D_B326_41CA_83A6BA138E24.html =
The answer is porphyritic dolerite.
htmlText_D39EA163_A47D_B326_41CA_83A6BA138E24.html =
The answer is porphyritic dolerite.
htmlText_D39EA163_A47D_B326_41CA_83A6BA138E24.html =
The answer is porphyritic dolerite.
htmlText_D39EA163_A47D_B326_41CA_83A6BA138E24.html =
The answer is porphyritic dolerite.
htmlText_4E79E8ED_BB93_959D_41E2_A48DB701FE60.html =
The answer is a hyperbyssal intrusion with a two-stage cooling history.
htmlText_FF269892_A407_B1E6_41D7_F80C83ADD290.html =
The answer is felsic.
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Structural identification Button_4F3978C2_AC15_29D0_41DB_DA2F5BBE63FB.label = 2.2.3 - Structural identification Button_4F3EB8C2_AC15_29D0_41E4_F64971FC9CAA.label = 2.2.4 - Download structural data Button_4F3EB8C2_AC15_29D0_41E4_F64971FC9CAA_mobile.label = 2.2.4 - Download structural data Button_4F3E48C8_AC15_29D0_41DD_5380AC549BDC_mobile.label = 2.3.1 - Rock description Button_4F3E48C8_AC15_29D0_41DD_5380AC549BDC.label = 2.3.1 - Rock description Button_4F3F88C8_AC15_29D0_41D5_98472D61A711_mobile.label = 2.3.2 - Download the sedimentary log A - B Button_4F3F88C8_AC15_29D0_41D5_98472D61A711.label = 2.3.2 - Download the sedimentary log A - B Button_4F3F38C9_AC15_29D0_41B0_E4B691C77123.label = 2.3.3 - Download the sedimentary log C - D Button_4F3F38C9_AC15_29D0_41B0_E4B691C77123_mobile.label = 2.3.3 - Download the sedimentary log C - D Button_4F3FC8CA_AC15_29D0_41DD_34581BD54A67_mobile.label = 2.3.4 - Rock description Button_4F3FC8CA_AC15_29D0_41DD_34581BD54A67.label = 2.3.4 - Rock 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Button_F42A806B_E1BE_7FB3_41E2_671D1204875F.label = 3.2.1 - Structural measurement Button_F42A806B_E1BE_7FB3_41E2_671D1204875F_mobile.label = 3.2.1 - Structural measurement Button_F42AD070_E1BE_7FAD_41EB_C4E8B1822834_mobile.label = 3.3.1 - Rock description Button_F42AD070_E1BE_7FAD_41EB_C4E8B1822834.label = 3.3.1 - Rock description Button_F42AA071_E1BE_7FAF_41E3_65E2769B40D1.label = 3.3.2 - Download structural data Button_F42AA071_E1BE_7FAF_41E3_65E2769B40D1_mobile.label = 3.3.2 - Download structural data Button_2D0F340A_E3BA_877D_41B6_8E7A6B1B8E8F.label = 4.0.1 - Introduction video Button_E31E1836_E276_8F95_41D2_F3E52099D59A.label = 4.0.1 - Introduction video Button_E31E0EA9_E276_80BF_41CB_CB6E7A2AB589.label = 4.0.1 - Introduction video Button_2D0F340A_E3BA_877D_41B6_8E7A6B1B8E8F_mobile.label = 4.0.1 - Introduction video Button_E31E0EA9_E276_80BF_41CB_CB6E7A2AB589_mobile.label = 4.0.1 - Introduction video Button_E31E1836_E276_8F95_41D2_F3E52099D59A_mobile.label = 4.0.1 - Introduction video Button_E31E327A_E276_839D_41E3_75209F605457.label = 4.0.2 - Introduction video Button_E31E3D42_E276_81ED_41DA_789E1EA9A05C.label = 4.0.2 - Introduction video Button_2D0F740B_E3BA_8773_41C9_543442141A34_mobile.label = 4.0.2 - Introduction video Button_2D0F740B_E3BA_8773_41C9_543442141A34.label = 4.0.2 - Introduction video Button_E31E327A_E276_839D_41E3_75209F605457_mobile.label = 4.0.2 - Introduction video Button_E31E3D42_E276_81ED_41DA_789E1EA9A05C_mobile.label = 4.0.2 - Introduction video Button_2D0F840C_E3BA_8775_41E7_25E737CBEC0C_mobile.label = 4.1.1 - Rock description and classification Button_2D0F840C_E3BA_8775_41E7_25E737CBEC0C.label = 4.1.1 - Rock description and classification Button_2D0FA40D_E3BA_8777_41E6_20A68EE868B2_mobile.label = 4.1.2 - Interpreting how rock units formed Button_2D0FA40D_E3BA_8777_41E6_20A68EE868B2.label = 4.1.2 - Interpreting how rock units formed Button_2D0FE40D_E3BA_8777_419C_9F0560B145CF.label = 4.1.3 - Rock description Button_2D0FE40D_E3BA_8777_419C_9F0560B145CF_mobile.label = 4.1.3 - Rock description Button_2D0F940E_E3BA_8775_41CD_F7E7C7107177_mobile.label = 4.1.4 - Rock description and classification Button_2D0F940E_E3BA_8775_41CD_F7E7C7107177.label = 4.1.4 - Rock description and classification Button_2D0FC40F_E3BA_8773_41D0_4175112FA50C.label = 4.1.5 - Boundary identification Button_2D0FC40F_E3BA_8773_41D0_4175112FA50C_mobile.label = 4.1.5 - Boundary identification Button_2D0FC410_E3BA_876D_41E1_33D41125E910_mobile.label = 4.1.6 - Rock description and classification Button_2D0FC410_E3BA_876D_41E1_33D41125E910.label = 4.1.6 - Rock description and classification Button_01F2D9B2_E3F5_80AD_41EA_F572E945B3D5.label = 4.1.7 - Rock description and classification Button_01F2D9B2_E3F5_80AD_41EA_F572E945B3D5_mobile.label = 4.1.7 - Rock description and classification Button_04E5E3A7_E3CA_80B3_41E2_D21BE35BE96E_mobile.label = 4.1.8 - Field relationships among rack units Button_04E5E3A7_E3CA_80B3_41E2_D21BE35BE96E.label = 4.1.8 - Field relationships among rack units Button_2D000410_E3BA_876D_41BF_548465012BC9.label = 4.1.9 - Rock description and classification Button_2D000410_E3BA_876D_41BF_548465012BC9_mobile.label = 4.1.9 - Rock description and classification Button_05504F71_E3CD_81AF_41D4_57DA9B2D3A18_mobile.label = 4.2.1 - Interpreting how rock units formed Button_05504F71_E3CD_81AF_41D4_57DA9B2D3A18.label = 4.2.1 - Interpreting how rock units formed Button_0A03B46C_E3CA_87B5_4195_60D5065E1E07_mobile.label = 4.2.2 - Interpreting how rock units formed Button_0A03B46C_E3CA_87B5_4195_60D5065E1E07.label = 4.2.2 - Interpreting how rock units formed Button_08FFD819_E3CA_8F9F_41E1_94A1B094D732.label = 4.2.3 - Interpreting how rock units formed Button_08FFD819_E3CA_8F9F_41E1_94A1B094D732_mobile.label = 4.2.3 - Interpreting how rock units formed Button_098A5F4A_E3CA_81FD_41D6_474E534A221F_mobile.label = 4.2.4 - Interpreting how rock units formed Button_098A5F4A_E3CA_81FD_41D6_474E534A221F.label = 4.2.4 - Interpreting how rock units formed Button_0E3F2C12_E3CB_876D_41E8_95A2D2AA926C_mobile.label = 4.2.5 - Plotting structural data to download Button_0E3F2C12_E3CB_876D_41E8_95A2D2AA926C.label = 4.2.5 - Plotting structural data to download and plot Button_0CC070EC_E3CB_80B5_41D3_03D2EA3D0A80.label = 4.2.6 - Interpreting how rock units formed Button_0CC070EC_E3CB_80B5_41D3_03D2EA3D0A80_mobile.label = 4.2.6 - Interpreting how rock units formed Button_0D65C81D_E3CB_8F97_41C7_2D8C65E44CDB.label = 4.2.7 - Interpreting how rock units formed Button_0D65C81D_E3CB_8F97_41C7_2D8C65E44CDB_mobile.label = 4.2.7 - Interpreting how rock units formed Button_3D3279E7_E3CA_80B3_41D9_6E7AEC0FE8B3_mobile.label = 4.2.8 - Interpreting how rock units formed Button_3D3279E7_E3CA_80B3_41D9_6E7AEC0FE8B3.label = 4.2.8 - Interpreting how rock units formed Button_0AE6E8DD_E3CD_8097_41E2_6CC36E1E9637_mobile.label = 4.3.1 - Petrographic description and interpretation Button_0AE6E8DD_E3CD_8097_41E2_6CC36E1E9637.label = 4.3.1 - Petrographic description and interpretation Button_0BA48EBA_E3CA_809D_41DC_C605BB099F79_mobile.label = 4.3.2 - Interpret geochemistry data Button_0BA48EBA_E3CA_809D_41DC_C605BB099F79.label = 4.3.2 - Interpret geochemistry data in context of field Button_089B93A1_E3CA_80AF_41E9_4B74505FA0FE_mobile.label = 4.3.3 - Petrographic description and interpretation Button_089B93A1_E3CA_80AF_41E9_4B74505FA0FE.label = 4.3.3 - Petrographic description and interpretation Button_0932DBF9_E3CA_809F_41DC_9A1A8E0D1522_mobile.label = 4.3.4 - Interpret geochemistry data Button_0932DBF9_E3CA_809F_41DC_9A1A8E0D1522.label = 4.3.4 - Interpret geochemistry data in context of field relationships Button_0D9CBC87_EC0F_7F59_41E8_2D28E81A721D_mobile.label = 5.0.1 - Introduction video A Button_0DF2F6DA_EC0F_48EB_41D6_5E604FB2C82D_mobile.label = 5.0.1 - Introduction video A Button_0C892049_E3D6_7FFF_41D3_B58F988E0B7F.label = 5.0.1 - Introduction video A Button_0D9CBC87_EC0F_7F59_41E8_2D28E81A721D.label = 5.0.1 - Introduction video A Button_0C892049_E3D6_7FFF_41D3_B58F988E0B7F_mobile.label = 5.0.1 - Introduction video A Button_0DF2F6DA_EC0F_48EB_41D6_5E604FB2C82D.label = 5.0.1 - Introduction video A Button_0C89F04A_E3D6_7FFD_41E2_1CD3540A4C68_mobile.label = 5.0.2 - Introduction video B Button_0C0B6901_EC0F_D959_41C7_5BEBC8943767_mobile.label = 5.0.2 - Introduction video B Button_0C0B6901_EC0F_D959_41C7_5BEBC8943767.label = 5.0.2 - Introduction video B Button_0CA91E70_EC0F_BBB7_41EC_82D83DF643FC_mobile.label = 5.0.2 - Introduction video B Button_0CA91E70_EC0F_BBB7_41EC_82D83DF643FC.label = 5.0.2 - Introduction video B Button_0C89F04A_E3D6_7FFD_41E2_1CD3540A4C68.label = 5.0.2 - Introduction video B Button_0C89304B_E3D6_7FF3_41CC_BBD11AA573E8.label = 5.1.1 - Relative timing Button_0C89304B_E3D6_7FF3_41CC_BBD11AA573E8_mobile.label = 5.1.1 - Relative timing Button_0C89604B_E3D6_7FF3_41E9_EC2EF875DB52.label = 5.1.2 - Rock description video Button_0C89604B_E3D6_7FF3_41E9_EC2EF875DB52_mobile.label = 5.1.2 - Rock description video Button_0C89204C_E3D6_7FF5_41DE_6CBD70CAD5E0_mobile.label = 5.1.3 - Structural measurements Button_0C89204C_E3D6_7FF5_41DE_6CBD70CAD5E0.label = 5.1.3 - Structural measurements Button_0C89704D_E3D6_7FF7_41E8_62C8CB187934_mobile.label = 5.1.4 - Describing structures Button_0C89704D_E3D6_7FF7_41E8_62C8CB187934.label = 5.1.4 - Describing structures Button_0A0D98CB_EC03_58E9_41E2_50842E8CF6CC_mobile.label = 5.2.1 - Measuring elements of a fold video Button_0A0D98CB_EC03_58E9_41E2_50842E8CF6CC.label = 5.2.1 - Measuring elements of a fold video Button_32D95066_EC01_C7DB_41CD_CC70F4872A25.label = 5.2.2 - Describing fold elements in the field Button_32D95066_EC01_C7DB_41CD_CC70F4872A25_mobile.label = 5.2.2 - Describing fold elements in the field Button_0DD89E9F_EC01_FB69_41B8_99B09974C4AC_mobile.label = 5.2.3 - Structural data to download and plot Button_0DD89E9F_EC01_FB69_41B8_99B09974C4AC.label = 5.2.3 - Structural data to download and plot Button_0CF9DB40_EC01_B9D7_41DA_9F5A40F18B26.label = 5.2.4 - Measuring structures Button_0CF9DB40_EC01_B9D7_41DA_9F5A40F18B26_mobile.label = 5.2.4 - Measuring structures Button_0F8C32FD_EC01_48A9_41EC_00DBD5C57F12_mobile.label = 5.2.5 - Measuring and classifying folds Button_0F8C32FD_EC01_48A9_41EC_00DBD5C57F12.label = 5.2.5 - Measuring and classifying folds Button_0E87E14A_EC01_49EB_41E1_FF823B8D56EB.label = 5.2.6 - Structural data to download and plot Button_0E87E14A_EC01_49EB_41E1_FF823B8D56EB_mobile.label = 5.2.6 - Structural data to download and plot Button_04FF3AEB_EC06_D8A9_41EB_DF43484EBF61_mobile.label = 5.2.7 - Measuring structures Button_04FF3AEB_EC06_D8A9_41EB_DF43484EBF61.label = 5.2.7 - Measuring structures Button_073A9FA3_EC01_5959_41E6_81B5679222E1.label = 5.2.8 - Structural data to download and plot Button_073A9FA3_EC01_5959_41E6_81B5679222E1_mobile.label = 5.2.8 - Structural data to download and plot Button_093E0C5F_EC07_BFE9_41ED_705E790A5EFC.label = 5.2.9 - Making a map Button_093E0C5F_EC07_BFE9_41ED_705E790A5EFC_mobile.label = 5.2.9 - Making a map Button_06F7CED3_EC06_B8F9_41D3_562D89BB26E0_mobile.label = 5.3.1 - Old mine workings Button_06F7CED3_EC06_B8F9_41D3_562D89BB26E0.label = 5.3.1 - Old mine workings Button_08120645_EC03_4BD9_41D2_735E6907D165.label = 5.3.2 - Describing fold elements in the field Button_08120645_EC03_4BD9_41D2_735E6907D165_mobile.label = 5.3.2 - Describing fold elements in the field Button_0B27EE9D_EC03_5B69_41EC_5387B67071EC_mobile.label = 5.3.3 - Measuring elements of a fold Button_0B27EE9D_EC03_5B69_41EC_5387B67071EC.label = 5.3.3 - Measuring elements of a fold Button_0A3A312E_EC03_C9AB_41EC_5EA855C81755.label = 5.3.4 - Interpretation of formation Button_0A3A312E_EC03_C9AB_41EC_5EA855C81755_mobile.label = 5.3.4 - Interpretation of formation Button_F2726882_F401_C75B_41E4_49696BAF929A_mobile.label = 6.0 - Introduction video Button_F2725DD7_F401_F8F9_41C9_BC384AB147BC_mobile.label = 6.0 - Introduction video Button_F2726882_F401_C75B_41E4_49696BAF929A.label = 6.0 - Introduction video Button_F2725DD7_F401_F8F9_41C9_BC384AB147BC.label = 6.0 - Introduction video Button_26B50A10_EC06_DB77_41E7_DE5820727049.label = 6.0 - Introduction video Button_26B50A10_EC06_DB77_41E7_DE5820727049_mobile.label = 6.0 - Introduction video Button_268ACA10_EC06_DB77_41D7_967CC6D707B2_mobile.label = 6.1.1 - Making geological sketches of rocks and their relationships Button_268ACA10_EC06_DB77_41D7_967CC6D707B2.label = 6.1.1 – Making geological sketches of rocks and their relationships Button_268A8A11_EC06_DB79_41B2_58A36432DDF0_mobile.label = 6.1.2 - Interpreting how rock units formed Button_268A8A11_EC06_DB79_41B2_58A36432DDF0.label = 6.1.2 – Interpreting how rock units formed Button_F2DAC87E_F406_C7AB_41E1_F5F44AE27535.label = 6.2.1 - Interpreting how rock units formed Button_F2DAC87E_F406_C7AB_41E1_F5F44AE27535_mobile.label = 6.2.1 - Interpreting how rock units formed Button_268B2A21_EC06_DB59_41D7_46E6C17AF891.label = 6.3.1 - Incorporating micro-scope-scale observation Button_268B2A21_EC06_DB59_41D7_46E6C17AF891_mobile.label = 6.3.1 - Incorporating micro-scope-scale observation Button_2688EA21_EC06_DB59_41E2_D8857FEFBE11_mobile.label = 6.3.2 - Interpret geochemistry data in context of field relationships Button_2688EA21_EC06_DB59_41E2_D8857FEFBE11.label = 6.3.2 - Interpret geochemistry data in context of field relationships Button_F2A9D712_F402_C97B_41E9_F3C20477D77D.label = 7.0 - Introduction video Button_F2A9D712_F402_C97B_41E9_F3C20477D77D_mobile.label = 7.0 - Introduction video Button_F2A9F684_F402_CB5F_41E3_D9DEDA865BE3.label = 7.0 - Introduction video Button_F2A9F684_F402_CB5F_41E3_D9DEDA865BE3_mobile.label = 7.0 - Introduction video Button_27C103F9_EC06_C8A9_41C9_5983D60D10BC_mobile.label = 7.0 - Introduction video Button_27C103F9_EC06_C8A9_41C9_5983D60D10BC.label = 7.0 - Introduction video Button_27C193FA_EC06_C8AB_41DD_119118870821_mobile.label = 7.1.1 - Identify and classifying rocks based on descriptions Button_27C193FA_EC06_C8AB_41DD_119118870821.label = 7.1.1 - Identify and classifying rocks based on descriptions Button_F2A3F4DB_F406_C8E9_41E1_37FD1211F1EB_mobile.label = 7.1.2 - Identify and classifying rocks based on descriptions Button_F2A3F4DB_F406_C8E9_41E1_37FD1211F1EB.label = 7.1.2 - Identify and classifying rocks based on descriptions Button_27C153FB_EC06_C8A9_41E1_A608157138B7.label = 7.1.3 - Identify and classifying rocks based on descriptions Button_27C153FB_EC06_C8A9_41E1_A608157138B7_mobile.label = 7.1.3 - Identify and classifying rocks based on descriptions Button_27C15402_EC06_CF5B_41CC_6182AC0C9E80_mobile.label = 7.2.1 - Geological history from field observation Button_27C15402_EC06_CF5B_41CC_6182AC0C9E80.label = 7.2.1 - Geological history from field observation Button_27C11403_EC06_CF59_41D6_01C1F7E68F7C_mobile.label = 7.2.2 - Interpreting relationships from a field map Button_27C11403_EC06_CF59_41D6_01C1F7E68F7C.label = 7.2.2 - Interpreting relationships from a field map Button_27C7B409_EC06_CF69_41A9_F48A9701164F.label = 7.3.1 - Incorporating micro-scope-scale observation Button_27C7B409_EC06_CF69_41A9_F48A9701164F_mobile.label = 7.3.1 - Incorporating micro-scope-scale observation Button_27C7740A_EC06_CF6B_41EC_1E83EB6E89A1.label = 7.3.2 - Incorporating micro-scope-scale observation Button_27C7740A_EC06_CF6B_41EC_1E83EB6E89A1_mobile.label = 7.3.2 - Incorporating micro-scope-scale observation Button_27C7B40A_EC06_CF6B_41E0_E5158DD56B1F.label = 7.3.3 - Interpret geochemistry data in context of field relationships Button_27C7B40A_EC06_CF6B_41E0_E5158DD56B1F_mobile.label = 7.3.3 - Interpret geochemistry data in context of field relationships Button_F2EE3037_F401_47B9_41CC_4C5843D92C09_mobile.label = 8.0 - Introduction video 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Credits



Nick Timms (Curtin EPS) – mastermind and overlord and acknowledges support from a Curtin Media Grant


Madelon Heperi (Curtin FLET) – programming, graphic design and teaching and learning design


Martin Towner (Curtin EPS) – drone pilot, cameraman, sound guy, field model, drone mosaic data processing


Aaron Cavosie (Curtin EPS) – geochemistry data and petrology wizard


Katy Evans (Curtin EPS) – teaching and learning design and acknowledges support from a Curtin Media Grant


Diana Taylor (Curtin FLET) – teaching and learning design


David Mole (CSRIO at the time) – whole geochemistry and sample collector and acknowledges support from the Science Plus Leader program of CSIRO


Chris Kirkland (Curtin EPS) – geochronology data collection and processing


Sean Makin (Curtin EPS) – drone pilot and data processing


Andrea Rajšic (Curtin EPS) – 360 camera operator, structural data collection and field model


Dave Belton (Curtin EPS) – areal 360 drone pilot and data processing


Tony Snow (Curtin EPS) – areal 360 drone co-pilot and assistant


Denis Fougerouse (Curtin EPS) – field model


Timmons Erickson (Curtin EPS, now at NASA) – sample collector


Steve Reddy (Curtin EPS) – sample collector
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Credits



Nick Timms (Curtin EPS) – mastermind and overlord and acknowledges support from a Curtin Media Grant


Madelon Heperi (Curtin FLET) – programming, graphic design and teaching and learning design


Martin Towner (Curtin EPS) – drone pilot, cameraman, sound guy, field model, drone mosaic data processing


Aaron Cavosie (Curtin EPS) – geochemistry data and petrology wizard


Katy Evans (Curtin EPS) – teaching and learning design and acknowledges support from a Curtin Media Grant


Diana Taylor (Curtin FLET) – teaching and learning design


David Mole (CSRIO at the time) – whole geochemistry and sample collector and acknowledges support from the Science Plus Leader program of CSIRO


Chris Kirkland (Curtin EPS) – geochronology data collection and processing


Sean Makin (Curtin EPS) – drone pilot and data processing


Andrea Rajšic (Curtin EPS) – 360 camera operator, structural data collection and field model


Dave Belton (Curtin EPS) – areal 360 drone pilot and data processing


Tony Snow (Curtin EPS) – areal 360 drone co-pilot and assistant


Denis Fougerouse (Curtin EPS) – field model


Timmons Erickson (Curtin EPS, now at NASA) – sample collector


Steve Reddy (Curtin EPS) – sample collector
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Header 1


Header 2 [Youtube]


[Dev note: this is an embedded YouTube movie with the suggested videos disabled and autoplay. Autoplay will only work on Desktop computers not on mobile devices]
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Integer gravida dui quis euismod placerat. Maecenas quis accumsan ipsum. Aliquam gravida velit at dolor mollis, quis luctus mauris vulputate. Proin condimentum id nunc sed sollicitudin.


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Header 1


Header 2 [Youtube]


[Dev note: this is an embedded YouTube movie with the suggested videos disabled and autoplay. Autoplay will only work on Desktop computers not on mobile devices]
Mauris aliquet neque quis libero consequat vestibulum. Donec lacinia consequat dolor viverra sagittis. Praesent consequat porttitor risus, eu condimentum nunc. Proin et velit ac sapien luctus efficitur egestas ac augue. Nunc dictum, augue eget eleifend interdum, quam libero imperdiet lectus, vel scelerisque turpis lectus vel ligula. Duis a porta sem. Maecenas sollicitudin nunc id risus fringilla, a pharetra orci iaculis. Aliquam turpis ligula, tincidunt sit amet consequat ac, imperdiet non dolor.


Integer gravida dui quis euismod placerat. Maecenas quis accumsan ipsum. Aliquam gravida velit at dolor mollis, quis luctus mauris vulputate. Proin condimentum id nunc sed sollicitudin.


Header 2


Nisl nec mi sollicitudin facilisis
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• Ut eget lorem sed leo.
• Sollicitudin tempor sit amet non urna.
• Aliquam feugiat mauris sit amet.
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Credits


Nick Timms (Curtin EPS) – mastermind, overlord and acknowledges support from a Curtin Media Grant


Madelon Heperi (Curtin FLET) – programming, graphic design and teaching and learning design


Martin Towner (Curtin EPS) – drone pilot, cameraman, sound guy, field model, drone mosaic data processing


Aaron Cavosie (Curtin EPS) – geochemistry data and petrology wizard


Katy Evans (Curtin EPS) – teaching and learning design and acknowledges support from a Curtin Media Grant


Diana Taylor (Curtin FLET) – teaching and learning design


David Mole (CSRIO at the time) – whole geochemistry and sample collector and acknowledges support from the Science Plus Leader program of CSIRO


Chris Kirkland (Curtin EPS) – geochronology data collection and processing


Sean Makin (Curtin EPS) – drone pilot and data processing


Andrea Rajšic (Curtin EPS) – 360 camera operator, structural data collection and field model


Dave Belton (Curtin EPS) – areal 360 drone pilot and data processing


Tony Snow (Curtin EPS) – areal 360 drone co-pilot and assistant


Denis Fougerouse (Curtin EPS) – field model


Timmons Erickson (Curtin EPS, now at NASA) – sample collector


Steve Reddy (Curtin EPS) – sample collector
HTMLText_79D330ED_0151_BCF4_4156_F01FB64A5F57.html =
Credits


Nick Timms (Curtin EPS) – mastermind, overlord and acknowledges support from a Curtin Media Grant


Madelon Heperi (Curtin FLET) – programming, graphic design and teaching and learning design


Martin Towner (Curtin EPS) – drone pilot, cameraman, sound guy, field model, drone mosaic data processing


Aaron Cavosie (Curtin EPS) – geochemistry data and petrology wizard


Katy Evans (Curtin EPS) – teaching and learning design and acknowledges support from a Curtin Media Grant


Diana Taylor (Curtin FLET) – teaching and learning design


David Mole (CSRIO at the time) – whole geochemistry and sample collector and acknowledges support from the Science Plus Leader program of CSIRO


Chris Kirkland (Curtin EPS) – geochronology data collection and processing


Sean Makin (Curtin EPS) – drone pilot and data processing


Andrea Rajšic (Curtin EPS) – 360 camera operator, structural data collection and field model


Dave Belton (Curtin EPS) – areal 360 drone pilot and data processing


Tony Snow (Curtin EPS) – areal 360 drone co-pilot and assistant


Denis Fougerouse (Curtin EPS) – field model


Timmons Erickson (Curtin EPS, now at NASA) – sample collector


Steve Reddy (Curtin EPS) – sample collector
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Instructions for locality 1


Click the explore location 1 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
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Instructions for locality 1


Click the explore location 1 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
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Instructions for locality 2


Click the explore location 2 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_F43A2056_E1BE_7F95_41C8_545F3A3A6D5D.html =
Instructions for locality 3


Click the explore location 3 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_2D0E0406_E3BA_8775_41DA_34D51E89F129.html =
Instructions for locality 4


Click the explore location 4 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
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Instructions for locality 5


Click the explore location 5 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_0C8CE044_E3D6_7FF5_41E7_F1D5FDB0D1DD.html =
Instructions for locality 5


Click the explore location 5 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
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Instructions for locality 6


Click the explore location 5 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
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Instructions for locality 7


Click the explore location 7 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_24DEB9CE_EC01_D8EB_41A9_BDBB3D8E9D63.html =
Instructions for locality 8


Click the explore location 8 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_26B45A0B_EC06_DB69_414D_A8515E9C7A25_mobile.html =
Instructions for locality 6


Click the explore location 5 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_F43A2056_E1BE_7F95_41C8_545F3A3A6D5D_mobile.html =
Instructions for locality 3


Click the explore location 3 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_2D0E0406_E3BA_8775_41DA_34D51E89F129_mobile.html =
Instructions for locality 4


Click the explore location 4 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_0C8CE044_E3D6_7FF5_41E7_F1D5FDB0D1DD_mobile.html =
Instructions for locality 5


Click the explore location 5 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_27CC73F5_EC06_C8B9_4187_81F5A0FABC66_mobile.html =
Instructions for locality 7


Click the explore location 7 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
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Instructions for locality 8


Click the explore location 8 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
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Instructions


subtitle


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Donec feugiat:


• Nisl nec mi sollicitudin facilisis
• Nam sed faucibus est.
• Ut eget lorem sed leo.
• Sollicitudin tempor sit amet non
• Aliquam feugiat mauris sit amet.
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Instructions


Step 1
Download the base map files for locality 8.


Step 2
Print the subdued colour base map to fit to an A3 page.


Step 3
Carefully trace the margins of as many pillows as you can observe at this locality. Tip – use the strong colour base map on a screen to zoom in to see the image in detail. Add line symbols to your legend.


Step 4
Use keel and dome shapes of mapped pillows to annotate your map with younging symbols in appropriate orientations, and add to the legend.


HTMLText_9A481CCE_CDB7_A9F4_41BA_ABEEF518AC1D.html =
Instructions


Step 1
Download the base map files for locality 8.


Step 2
Print the subdued colour base map to fit to an A3 page.


Step 3
Carefully trace the margins of as many pillows as you can observe at this locality. Tip – use the strong colour base map on a screen to zoom in to see the image in detail. Add line symbols to your legend.


Step 4
Use keel and dome shapes of mapped pillows to annotate your map with younging symbols in appropriate orientations, and add to the legend.


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Instructions


Structural data and plot


Download the spreadsheet of the structural data and plot them on the base map Locality 2.
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Aerial views
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Aerial views
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Location


Mount Hunt


Yikari WA 6430
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Instructions


Step 1
Download the Base map files for locality 5.


Step 2
Find the data spreadsheets and plot data on the geology map.


Step 3
Infer bedrock geology boundaries through cover (scree and colluvium) on the geology map


Step 4
Infer any faults and large scale folds
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Instructions


These optical photomicrographs are from samples within 50m of this location.


Step 1
In a notebook, make petrographic descriptions of each sample, including mineralogy and texture, and identify rock types.


Step 2
Make interpretations about magmatic history, noting any possible petrogenetic links between the samples.


Step 3
Map the rock types on to the base map for this locality
HTMLText_C8133AC5_FD36_4C29_41D8_6A46CE980A97.html =
Instructions


These optical photomicrographs are from samples within 50m of this location.


Step 1
In a notebook, make petrographic descriptions of each sample, including mineralogy and texture, and identify rock types.


Step 2
Make interpretations about magmatic history, noting any possible petrogenetic links between the samples.


Step 3
Map the rock types on to the base map for this locality
HTMLText_BE94C485_B891_FD8D_41C8_B7202B320F9A.html =
Instructions


These optical photomicrographs are from samples within 50m of this location.


Step 1
In a notebook, make petrographic descriptions of each sample, including mineralogy and texture, and identify rock types.


Step 2
Make interpretations about magmatic history, noting any possible petrogenetic links between the samples.


Step 3
Map the rock types on to the base map for this locality
HTMLText_90C74282_B8B1_9587_41E6_A3033A71147F.html =
Instructions


Interpretation of formation environment


Download the sedimentary log and complete an interpretation of the environment of formation of the beds.
HTMLText_BE801F19_BB70_8C85_41D3_54AC77537042.html =
Instructions


Plotting structural data to download and plot


Download the spreadsheet of structural data and plot them on the base map for Locality 4 and a stereonet.
HTMLText_9A2B2EEB_B8B0_8D85_41DA_C3FA31A99E0E.html =
Instructions



Interpretation of formation environment


Download the sedimentary log and complete an interpretation of the environment of formation of the beds.
HTMLText_3D37CA66_B970_948F_41D7_CD7BF922FA64.html =
Instructions



Structural data to download and plot


Download the spreadsheet of the structural data and plot them on the base map Locality 3.
HTMLText_9522B7C7_CDFC_A7F4_41D9_B662F79CA8A7.html =
Instructions


Download the spreadsheet of the structural data and plot them on the base map Locality 2.
HTMLText_ADB0EFAC_CDFC_67B4_41DB_08D05E8D89CD.html =
Instructions


Download the spreadsheet of the structural data and plot them on the base map Locality 2.
HTMLText_E38766EF_9F7E_8540_41DB_FFEEA381D07B.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
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LOREM IPSUM


Mauris aliquet neque quis libero consequat vestibulum. Donec lacinia consequat dolor viverra sagittis. Praesent consequat porttitor risus, eu condimentum nunc. Proin et velit ac sapien luctus efficitur egestas ac augue. Nunc dictum, augue eget eleifend interdum, quam libero imperdiet lectus, vel scelerisque turpis lectus vel ligula. Duis a porta sem. Maecenas sollicitudin nunc id risus fringilla, a pharetra orci iaculis. Aliquam turpis ligula, tincidunt sit amet consequat ac, imperdiet non dolor.


HTMLText_E65110A3_9F43_9DC0_41D0_D96707610F81.html =
Instructions


Download the spreadsheets of structural data and plot them on the base map for locality 1.


HTMLText_80703397_C35B_5579_41D1_33A43CF1C780.html =
Instructions


Bedding data


Download the spreadsheet of structural data and plot them on the base map for Locality 5.


HTMLText_952F9649_C2DB_5FE9_41E6_DF2F081D836C.html =
Instructions


Foliation data


Download the spreadsheet of structural data and plot them on the base map for Locality 5.


HTMLText_88E22DFA_CC94_AB9C_41AF_11CF51B1C3DA.html =
Instructions


Interpreting how rock are formed


Download the image and make an interpretive sketch of the pillows at this location, making particular note of domes and keels.


HTMLText_B5A58B32_8030_A3D0_41DF_E338580D79AD.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality


HTMLText_BF307766_B990_9C8F_41B5_F2B8CDBC5E08.html =
Instructions


Structural data and plot


Download the spreadsheet of structural data and plot them on the base map for Locality 5.


HTMLText_E8057D40_80D0_67B0_41CA_3A38E159CD84.html =
Localities


There are eight localities of interest with various tasks and activities covering a range of skill levels.


Select the locality below that you want to explore than select the skill set relevant to that locality.
HTMLText_E6C344FC_9F42_8540_41DE_3B222EAAF757.html =
Instructions


Download the spreadsheets of structural data and plot them on the base map for locality 1.


HTMLText_80DE42D9_C35B_54E9_41D1_B133CE8CFF6C.html =
Instructions


Bedding data


Download the spreadsheet of structural data and plot them on the base map for Locality 5.


HTMLText_A472C1BB_CD8C_7B9C_41E0_733804FD89A3.html =
Instructions


Foliation data


Download the image and make an interpretive sketch of the pillows at this location, making particular note of domes and keels.


HTMLText_9622288D_C2DF_3369_41CD_2FC88B5AA64B.html =
Instructions


Foliation data


Download the spreadsheet of structural data and plot them on the base map for Locality 5.


HTMLText_AFD88AF3_CD95_A9AC_41E6_D965F41069E9.html =
Instructions


Interpreting how rock units formed


Download the image and make an interpretive sketch of the pillows at this location, making particular note of domes and keels.


HTMLText_BD74265C_8073_E250_41D4_5A5FBABD0659.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
HTMLText_E6C11502_9F42_84C0_41DD_7A529B6B5935.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
HTMLText_80DEC2E0_C35B_54D7_41B1_2143A941D645.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
HTMLText_BF3B044B_B990_7C85_41D1_C006B0925AB7.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
HTMLText_AFDA1AF9_CD95_A99C_41D8_C7A890004229.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
HTMLText_96232894_C2DF_337F_41D7_EA67CB0E452E.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
HTMLText_A44D01C0_CD8C_7BEC_41E8_FC0E37626C56.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
HTMLText_DE3723A8_95E8_3EF7_41E2_120BC0DE0F67.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality


HTMLText_BF3B0444_B990_7C83_41E3_338855844A47.html =
Instructions


Structural data and plot


Download the spreadsheet of structural data and plot them on the base map for Locality 5.


HTMLText_E8057D40_80D0_67B0_41CA_3A38E159CD84_mobile.html =
Localities


There are eight localities of interest with various tasks and activities covering a range of skill levels.


Select the locality below that you want to explore than select the skill set relevant to that locality.
HTMLText_4F3AC8B5_AC15_29B0_41D9_DD87B90C6EA5_mobile.html =
Instructions for locality 2


Click the explore location 2 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
HTMLText_BB3CB7DB_C2EF_5CE9_41AC_7F3655EACF18.html =
Instructions


Step 1
Download the Base map files for locality 5.


Step 2
Find the data spreadsheets and plot data on the geology map.


Step 3
Infer bedrock geology boundaries through cover (scree and colluvium) on the geology map


Step 4
Infer any faults and large scale folds











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Location


Mount Hunt


Yikari WA 6430







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Photo Album or image


This is a photo album / image template with download buttons.









HTMLText_9883C170_B8B0_9483_41BC_887D82714F78.html =
Instructions



Interpretation of formation environment


Download the sedimentary log and complete an interpretation of the environment of formation of the beds.
HTMLText_96E241F0_B990_F783_41DC_60FD28B9E304.html =
Instructions



Interpretation of formation environment


Download the sedimentary log and complete an interpretation of the environment of formation of the beds.
HTMLText_40C275FC_BB70_9F83_41E4_38705AD01538.html =
Instructions


Plotting structural data to download and plot


Download the spreadsheet of structural data and plot them on the base map for Locality 4 and a stereonet.
HTMLText_E2DAE97B_9EC2_8F40_41C5_956C80CFE2F6.html =
Instructions


Step 1
Download the base map files for locality 1


Step 2
Print the subdued colour base map to fit an A3 page


Step 3
Use all the available information to make a geological map of this locality
HTMLText_3E117F91_B890_8B85_41D5_62822A5F8D95.html =
Instructions


Structural data to download and plot


Download the spreadsheet of the structural data and plot them on the base map locality 3.
HTMLText_2DC6B1BE_ABAC_BA27_41B7_556847B19CC4.html =
Instructions


Structural data and plot


Download the spreadsheet of the structural data and plot them on the base map Locality 2.
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Instructions


Step 1
Download the base map files for locality 8.


Step 2
Print the subdued colour base map to fit to an A3 page.


Step 3
Carefully trace the margins of as many pillows as you can observe at this locality. Tip – use the strong colour base map on a screen to zoom in to see the image in detail. Add line symbols to your legend.


Step 4
Use keel and dome shapes of mapped pillows to annotate your map with younging symbols in appropriate orientations, and add to the legend.
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360 VR Geological


This Virtual Geological Fieldtrip takes you to selected geological landmarks over two square kilometres of dry and harsh climate of Kalgoorlie Boulder, Western Australia.


With 360-degree panoramas, 3D photogrammetry, drone footage, microscopic images and datasheets this resource provides you with an array data required to carry out geological.


In the acitivy panoramas, select the level you would like to explore.


Credits


Curtin University
Faculty of Science and Engineering
Office of the Dean Teaching and Learning





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Instructions



These optical photomicrographs are from samples within 50m of this location.


Step 1
In a notebook, make petrographic descriptions of each sample, including mineralogy and texture, and identify rock types.


Step 2
Make interpretations about magmatic history, noting any possible petrogenetic links between the samples.


Step 3
Map the rock types on to the base map for this locality.
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Instructions



These optical photomicrographs are from samples within 50m of this location.


Step 1
In a notebook, make petrographic descriptions of each sample, including mineralogy and texture, and identify rock types.


Step 2
Make interpretations about magmatic history, noting any possible petrogenetic links between the samples.


Step 3
Map the rock types on to the base map for this locality.
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Instructions for locality 1


Click the explore location 1 button below OR from the tabs above choose a skill level: novice, intermediate or advanced level.


To find a specific skill use the contents tabs above, following a link will take you directly to the locality for that activity.


Remember to take your time observing the environment, explore it, describe it and map it.
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